TY  - JOUR
AU  - Batoćanin, Natalija
AU  - Wróblewski, Wojciech
AU  - Carević, Ivana
AU  - Durlević, Uroš
AU  - Gajić, Violeta
AU  - Valjarević, Aleksandar
PY  - 2023
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1187
AB  - Tufa accumulations from the Gostilje River Basin and the Sopotnica River Basin in SW Serbia are represented by both active and fossil tufa precipitates. The aim of this study is to distinguish and describe different tufa facies and to determine the environmental conditions, based on stable isotope data. We also compare our analysis with other tufa deposits in Europe. Four facies are distinguished: moss tufa, algal tufa, stromatolitic laminated tufa, and phytoclastic tufa. The dominant constituent of all tufa samples is low Mg-calcite, whereas the presence of sylvite is noted in two samples from the Gostilje River Basin. The δ18O values range from −9.07‰ to −10.79‰ (mean value: −9.81‰), while the δ13C values range from −6.50‰ to −10.34‰ (mean values −9.01‰). The stable isotope values (δ13C and δ18O) indicate that these tufa deposits were precipitated from cold, ambient water supported by CO2 of an atmospheric origin. We emphasize that this is the first data about stable isotope analyses of tufa deposits from Serbia.
PB  - MDPI, Basel
T2  - Applied Sciences
T1  - Facies and Origin of Tufa Deposits from the Gostilje River Basin and the Sopotnica River Basin (SW Serbia)
VL  - 13
IS  - 5
SP  - 3190
DO  - 10.3390/app13053190
ER  - 

@article{
author = "Batoćanin, Natalija and Wróblewski, Wojciech and Carević, Ivana and Durlević, Uroš and Gajić, Violeta and Valjarević, Aleksandar",
year = "2023",
abstract = "Tufa accumulations from the Gostilje River Basin and the Sopotnica River Basin in SW Serbia are represented by both active and fossil tufa precipitates. The aim of this study is to distinguish and describe different tufa facies and to determine the environmental conditions, based on stable isotope data. We also compare our analysis with other tufa deposits in Europe. Four facies are distinguished: moss tufa, algal tufa, stromatolitic laminated tufa, and phytoclastic tufa. The dominant constituent of all tufa samples is low Mg-calcite, whereas the presence of sylvite is noted in two samples from the Gostilje River Basin. The δ18O values range from −9.07‰ to −10.79‰ (mean value: −9.81‰), while the δ13C values range from −6.50‰ to −10.34‰ (mean values −9.01‰). The stable isotope values (δ13C and δ18O) indicate that these tufa deposits were precipitated from cold, ambient water supported by CO2 of an atmospheric origin. We emphasize that this is the first data about stable isotope analyses of tufa deposits from Serbia.",
publisher = "MDPI, Basel",
journal = "Applied Sciences",
title = "Facies and Origin of Tufa Deposits from the Gostilje River Basin and the Sopotnica River Basin (SW Serbia)",
volume = "13",
number = "5",
pages = "3190",
doi = "10.3390/app13053190"
}

Batoćanin, N., Wróblewski, W., Carević, I., Durlević, U., Gajić, V.,& Valjarević, A.. (2023). Facies and Origin of Tufa Deposits from the Gostilje River Basin and the Sopotnica River Basin (SW Serbia). in Applied Sciences
MDPI, Basel., 13(5), 3190.
https://doi.org/10.3390/app13053190

Batoćanin N, Wróblewski W, Carević I, Durlević U, Gajić V, Valjarević A. Facies and Origin of Tufa Deposits from the Gostilje River Basin and the Sopotnica River Basin (SW Serbia). in Applied Sciences. 2023;13(5):3190.
doi:10.3390/app13053190 .

Batoćanin, Natalija, Wróblewski, Wojciech, Carević, Ivana, Durlević, Uroš, Gajić, Violeta, Valjarević, Aleksandar, "Facies and Origin of Tufa Deposits from the Gostilje River Basin and the Sopotnica River Basin (SW Serbia)" in Applied Sciences, 13, no. 5 (2023):3190,
https://doi.org/10.3390/app13053190 . .

TY  - JOUR
AU  - Manojlović, Sanja
AU  - Sibinović, Mikica
AU  - Srejić, Tanja
AU  - Novković, Ivan
AU  - Milošević, Marko
AU  - Gatarić, Dragica
AU  - Carević, Ivana
AU  - Batoćanin, Natalija
PY  - 2022
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1153
AB  - The intensity of soil erosion is the result of a combined action of natural factors and different
human activities. This work aims to determine the factors controlling the change of soil
erosion. Eleven watersheds from different parts of Serbia were used as the study area. An
Erosion Potential Model was applied to estimate the soil erosion status of the watersheds
in two periods, 1971 and 2010. The model indicated that the reduction of soil erosion
intensity in the watersheds ranges from 12.4% to 82.7%. The statistical analysis examines
quantitative relationships and combined effects between soil erosion and socio-economic
and main physical-geographical determinants in watersheds. Watershed characteristics
were divided into 5 classes, and within each class 22 variables were calculated: two
variables relate to erosion, one to topography, two to land cover, seven to demographic
and ten to agrarian variables. Correlation analysis and Principal Component Analysis (PCA)
have been applied to understand the main variables that contribute to change soil erosion
intensity. The PCA identified four components that can explain at least up to 79.06% of the
variation of all variables. This study explores new indicators for correlations with changing
soil erosion and provides decision makers with access to quantification for environmental
impact assessment and decision-making for adequate soil conservation and management
programs.
PB  - Frontiers Media S.A., Lausanne, Switzerland
T2  - Frontiers in Environmental Science
T1  - Factors Controlling the Change of Soil Erosion Intensity in Mountain Watersheds in Serbia
VL  - 10
SP  - 888901
DO  - 10.3389/fenvs.2022.888901
ER  - 

@article{
author = "Manojlović, Sanja and Sibinović, Mikica and Srejić, Tanja and Novković, Ivan and Milošević, Marko and Gatarić, Dragica and Carević, Ivana and Batoćanin, Natalija",
year = "2022",
abstract = "The intensity of soil erosion is the result of a combined action of natural factors and different
human activities. This work aims to determine the factors controlling the change of soil
erosion. Eleven watersheds from different parts of Serbia were used as the study area. An
Erosion Potential Model was applied to estimate the soil erosion status of the watersheds
in two periods, 1971 and 2010. The model indicated that the reduction of soil erosion
intensity in the watersheds ranges from 12.4% to 82.7%. The statistical analysis examines
quantitative relationships and combined effects between soil erosion and socio-economic
and main physical-geographical determinants in watersheds. Watershed characteristics
were divided into 5 classes, and within each class 22 variables were calculated: two
variables relate to erosion, one to topography, two to land cover, seven to demographic
and ten to agrarian variables. Correlation analysis and Principal Component Analysis (PCA)
have been applied to understand the main variables that contribute to change soil erosion
intensity. The PCA identified four components that can explain at least up to 79.06% of the
variation of all variables. This study explores new indicators for correlations with changing
soil erosion and provides decision makers with access to quantification for environmental
impact assessment and decision-making for adequate soil conservation and management
programs.",
publisher = "Frontiers Media S.A., Lausanne, Switzerland",
journal = "Frontiers in Environmental Science",
title = "Factors Controlling the Change of Soil Erosion Intensity in Mountain Watersheds in Serbia",
volume = "10",
pages = "888901",
doi = "10.3389/fenvs.2022.888901"
}

Manojlović, S., Sibinović, M., Srejić, T., Novković, I., Milošević, M., Gatarić, D., Carević, I.,& Batoćanin, N.. (2022). Factors Controlling the Change of Soil Erosion Intensity in Mountain Watersheds in Serbia. in Frontiers in Environmental Science
Frontiers Media S.A., Lausanne, Switzerland., 10, 888901.
https://doi.org/10.3389/fenvs.2022.888901

Manojlović S, Sibinović M, Srejić T, Novković I, Milošević M, Gatarić D, Carević I, Batoćanin N. Factors Controlling the Change of Soil Erosion Intensity in Mountain Watersheds in Serbia. in Frontiers in Environmental Science. 2022;10:888901.
doi:10.3389/fenvs.2022.888901 .

Manojlović, Sanja, Sibinović, Mikica, Srejić, Tanja, Novković, Ivan, Milošević, Marko, Gatarić, Dragica, Carević, Ivana, Batoćanin, Natalija, "Factors Controlling the Change of Soil Erosion Intensity in Mountain Watersheds in Serbia" in Frontiers in Environmental Science, 10 (2022):888901,
https://doi.org/10.3389/fenvs.2022.888901 . .

TY  - JOUR
AU  - Carević, Ivana
AU  - Sibinović, Mikica
AU  - Manojlović, Sanja
AU  - Batoćanin, Natalija
AU  - Petrović, Aleksandar S.
AU  - Srejić, Tanja
PY  - 2021
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1114
AB  - One of the biggest problems of environmental protection in Serbia is landfills. It is often a case that the economic interests are predominant in the landfill sitting; thus, most landfills are not located according to standards. This study shows that detailed geological data assets combined with geographical modeling represents a reliable way to define and locate the landfill site. Geological evaluation is discussed in detail with regard to bedrock lithology, quaternary geology, geological structure, hydrogeology, surface runoff patterns, and topography. An approach combining geographical modeling and geology is presented for determining the sites suitable for landfill selection with respect to their geologic favorability. As opposed to numerous research papers on this topic, in the methodological procedure, special importance is devoted to the analysis of the geological criteria. In this way, it is significantly easier to determine the landfill area with the best characteristics due to geological structure and lithology which unequivocally and precisely indicates inadequate territories for candidate sites. The multicriteria decision analysis (MCDA) is based on geological criteria upgraded with road (primary, residential, secondary, and tertiary), settlements network, railway, airport, infrastructure, land use, hypsometry aquifer, wetland, and surface water. The score values are divided into four classes, i.e., restricted areas, suitable but avoid, suitable, and most suitable. Combining geographical modeling with geology led to the recognition of two locations to be most favorable for landfill site located in the most suitable area, which represents 25.3% of the study area.
PB  - MDPI, Basel
T2  - Sustainability
T1  - Geological Approach for Landfill Site Selection: A Case Study of Vršac Municipality, Serbia
VL  - 13
IS  - 14
SP  - 7810
DO  - 10.3390/su13147810
UR  - https://hdl.handle.net/21.15107/rcub_gery_1114
ER  - 

@article{
author = "Carević, Ivana and Sibinović, Mikica and Manojlović, Sanja and Batoćanin, Natalija and Petrović, Aleksandar S. and Srejić, Tanja",
year = "2021",
abstract = "One of the biggest problems of environmental protection in Serbia is landfills. It is often a case that the economic interests are predominant in the landfill sitting; thus, most landfills are not located according to standards. This study shows that detailed geological data assets combined with geographical modeling represents a reliable way to define and locate the landfill site. Geological evaluation is discussed in detail with regard to bedrock lithology, quaternary geology, geological structure, hydrogeology, surface runoff patterns, and topography. An approach combining geographical modeling and geology is presented for determining the sites suitable for landfill selection with respect to their geologic favorability. As opposed to numerous research papers on this topic, in the methodological procedure, special importance is devoted to the analysis of the geological criteria. In this way, it is significantly easier to determine the landfill area with the best characteristics due to geological structure and lithology which unequivocally and precisely indicates inadequate territories for candidate sites. The multicriteria decision analysis (MCDA) is based on geological criteria upgraded with road (primary, residential, secondary, and tertiary), settlements network, railway, airport, infrastructure, land use, hypsometry aquifer, wetland, and surface water. The score values are divided into four classes, i.e., restricted areas, suitable but avoid, suitable, and most suitable. Combining geographical modeling with geology led to the recognition of two locations to be most favorable for landfill site located in the most suitable area, which represents 25.3% of the study area.",
publisher = "MDPI, Basel",
journal = "Sustainability",
title = "Geological Approach for Landfill Site Selection: A Case Study of Vršac Municipality, Serbia",
volume = "13",
number = "14",
pages = "7810",
doi = "10.3390/su13147810",
url = "https://hdl.handle.net/21.15107/rcub_gery_1114"
}

Carević, I., Sibinović, M., Manojlović, S., Batoćanin, N., Petrović, A. S.,& Srejić, T.. (2021). Geological Approach for Landfill Site Selection: A Case Study of Vršac Municipality, Serbia. in Sustainability
MDPI, Basel., 13(14), 7810.
https://doi.org/10.3390/su13147810
https://hdl.handle.net/21.15107/rcub_gery_1114

Carević I, Sibinović M, Manojlović S, Batoćanin N, Petrović AS, Srejić T. Geological Approach for Landfill Site Selection: A Case Study of Vršac Municipality, Serbia. in Sustainability. 2021;13(14):7810.
doi:10.3390/su13147810
https://hdl.handle.net/21.15107/rcub_gery_1114 .

Carević, Ivana, Sibinović, Mikica, Manojlović, Sanja, Batoćanin, Natalija, Petrović, Aleksandar S., Srejić, Tanja, "Geological Approach for Landfill Site Selection: A Case Study of Vršac Municipality, Serbia" in Sustainability, 13, no. 14 (2021):7810,
https://doi.org/10.3390/su13147810 .,
https://hdl.handle.net/21.15107/rcub_gery_1114 .

TY  - JOUR
AU  - Petrović, Aleksandar S.
AU  - Nikolić, Dragana
AU  - Trnavac-Bogdanović, Dušica
AU  - Carević, Ivana
PY  - 2020
UR  - https://gery.gef.bg.ac.rs/handle/123456789/1071
AB  - Protection and promotion of geoheritage has been changing and improving in recent decades, in line with the growing research in this field. Some research papers specifically study geomorphological geoheritage and introduce a special term - geomorphosite. Karst geomorphosites present specific objects of geomorphological heritage. On Kucaj and Beljanica mountains there is the largest karst area in Serbia. The purpose of this paper is to select and evaluate the scientific value of karst geomorphosites of Kucaj and Beljanica. More than one hundred karst geomorphosites were analyzed. In order to achieve more adequate coverage and representation, they were grouped into 25 geomorphotypes in three major geomorphological components of the investigated area. The results of this analysis highlighted the most important natural potentials of this area for establishing a karst-based geopark. More than 20 geomorphotypes have a positive recommendation index, which provides a good basis for further geotourism analysis.
PB  - Karst Research Inst Zrc Sazu, Postojna
T2  - Acta Carsologica
T1  - Assessment of karst geomorphosites on Kucaj and Beljanica mountains as a resource for the development of karst-based geopark
VL  - 49
IS  - 2-3
SP  - 179
EP  - 190
DO  - 10.3986/ac.v49i2-3.8748
UR  - https://hdl.handle.net/21.15107/rcub_gery_1071
ER  - 

@article{
author = "Petrović, Aleksandar S. and Nikolić, Dragana and Trnavac-Bogdanović, Dušica and Carević, Ivana",
year = "2020",
abstract = "Protection and promotion of geoheritage has been changing and improving in recent decades, in line with the growing research in this field. Some research papers specifically study geomorphological geoheritage and introduce a special term - geomorphosite. Karst geomorphosites present specific objects of geomorphological heritage. On Kucaj and Beljanica mountains there is the largest karst area in Serbia. The purpose of this paper is to select and evaluate the scientific value of karst geomorphosites of Kucaj and Beljanica. More than one hundred karst geomorphosites were analyzed. In order to achieve more adequate coverage and representation, they were grouped into 25 geomorphotypes in three major geomorphological components of the investigated area. The results of this analysis highlighted the most important natural potentials of this area for establishing a karst-based geopark. More than 20 geomorphotypes have a positive recommendation index, which provides a good basis for further geotourism analysis.",
publisher = "Karst Research Inst Zrc Sazu, Postojna",
journal = "Acta Carsologica",
title = "Assessment of karst geomorphosites on Kucaj and Beljanica mountains as a resource for the development of karst-based geopark",
volume = "49",
number = "2-3",
pages = "179-190",
doi = "10.3986/ac.v49i2-3.8748",
url = "https://hdl.handle.net/21.15107/rcub_gery_1071"
}

Petrović, A. S., Nikolić, D., Trnavac-Bogdanović, D.,& Carević, I.. (2020). Assessment of karst geomorphosites on Kucaj and Beljanica mountains as a resource for the development of karst-based geopark. in Acta Carsologica
Karst Research Inst Zrc Sazu, Postojna., 49(2-3), 179-190.
https://doi.org/10.3986/ac.v49i2-3.8748
https://hdl.handle.net/21.15107/rcub_gery_1071

Petrović AS, Nikolić D, Trnavac-Bogdanović D, Carević I. Assessment of karst geomorphosites on Kucaj and Beljanica mountains as a resource for the development of karst-based geopark. in Acta Carsologica. 2020;49(2-3):179-190.
doi:10.3986/ac.v49i2-3.8748
https://hdl.handle.net/21.15107/rcub_gery_1071 .

Petrović, Aleksandar S., Nikolić, Dragana, Trnavac-Bogdanović, Dušica, Carević, Ivana, "Assessment of karst geomorphosites on Kucaj and Beljanica mountains as a resource for the development of karst-based geopark" in Acta Carsologica, 49, no. 2-3 (2020):179-190,
https://doi.org/10.3986/ac.v49i2-3.8748 .,
https://hdl.handle.net/21.15107/rcub_gery_1071 .

TY  - JOUR
AU  - Rostami, Leila
AU  - Vaziri, Seyed Hamid
AU  - Jahani, Davood
AU  - Solgi, Ali
AU  - Abad, Morteza Taherpour Khalil
AU  - Carević, Ivana
AU  - Yahyaei, Ahmad
PY  - 2019
UR  - https://gery.gef.bg.ac.rs/handle/123456789/1018
AB  - The Fahliyan Formation of the Khami Group is the most important oil and gas reservoir in southwestern Iran. The formation attains a thickness of 435.5 m in the oil well X2 in Dorood oil field, Persian Gulf It is represented mainly by thin-bedded limestones. This formation unconformably overlies the evaporate late Jurassic Hith Formation and conformably underlies the Gadvan Formation. Integrated palaeontological and sedimentological studies supported by an analysis of 150 thin-sections led to the identification of 21 benthic foraminiferal genera dominated by agglutinated forms with an additional 8 algal genera. Two foraminiferal biozones of Berriasian through Hauterivian age include the Pseudochrysalidina (Dokhania) arabica acme zone and Pseudocyclammina lituus-Coscinoconus assemblage zone, and an algal zone includes the Salpingoporella annulata range zone have been recognized. The correlation of the lower Cretaceous petroleum source rock in the Persian Gulf with regions from Tethyan Realm is limited by the lack of the analog formation that can be used for comparison. In this way, the foraminiferal zones are correlated with coeval zones in south and southwest of Iran.
PB  - Islamic Azad University
T2  - Iranian Journal of Earth Sciences
T1  - Neocomian Fahliyan formation carbonates in the oil well X2 (Dorood oil field, Persian Gulf): Biostratigraphic data from benthic foraminifera and algae
VL  - 11
IS  - 3
SP  - 173
EP  - 182
UR  - https://hdl.handle.net/21.15107/rcub_gery_1018
ER  - 

@article{
author = "Rostami, Leila and Vaziri, Seyed Hamid and Jahani, Davood and Solgi, Ali and Abad, Morteza Taherpour Khalil and Carević, Ivana and Yahyaei, Ahmad",
year = "2019",
abstract = "The Fahliyan Formation of the Khami Group is the most important oil and gas reservoir in southwestern Iran. The formation attains a thickness of 435.5 m in the oil well X2 in Dorood oil field, Persian Gulf It is represented mainly by thin-bedded limestones. This formation unconformably overlies the evaporate late Jurassic Hith Formation and conformably underlies the Gadvan Formation. Integrated palaeontological and sedimentological studies supported by an analysis of 150 thin-sections led to the identification of 21 benthic foraminiferal genera dominated by agglutinated forms with an additional 8 algal genera. Two foraminiferal biozones of Berriasian through Hauterivian age include the Pseudochrysalidina (Dokhania) arabica acme zone and Pseudocyclammina lituus-Coscinoconus assemblage zone, and an algal zone includes the Salpingoporella annulata range zone have been recognized. The correlation of the lower Cretaceous petroleum source rock in the Persian Gulf with regions from Tethyan Realm is limited by the lack of the analog formation that can be used for comparison. In this way, the foraminiferal zones are correlated with coeval zones in south and southwest of Iran.",
publisher = "Islamic Azad University",
journal = "Iranian Journal of Earth Sciences",
title = "Neocomian Fahliyan formation carbonates in the oil well X2 (Dorood oil field, Persian Gulf): Biostratigraphic data from benthic foraminifera and algae",
volume = "11",
number = "3",
pages = "173-182",
url = "https://hdl.handle.net/21.15107/rcub_gery_1018"
}

Rostami, L., Vaziri, S. H., Jahani, D., Solgi, A., Abad, M. T. K., Carević, I.,& Yahyaei, A.. (2019). Neocomian Fahliyan formation carbonates in the oil well X2 (Dorood oil field, Persian Gulf): Biostratigraphic data from benthic foraminifera and algae. in Iranian Journal of Earth Sciences
Islamic Azad University., 11(3), 173-182.
https://hdl.handle.net/21.15107/rcub_gery_1018

Rostami L, Vaziri SH, Jahani D, Solgi A, Abad MTK, Carević I, Yahyaei A. Neocomian Fahliyan formation carbonates in the oil well X2 (Dorood oil field, Persian Gulf): Biostratigraphic data from benthic foraminifera and algae. in Iranian Journal of Earth Sciences. 2019;11(3):173-182.
https://hdl.handle.net/21.15107/rcub_gery_1018 .

Rostami, Leila, Vaziri, Seyed Hamid, Jahani, Davood, Solgi, Ali, Abad, Morteza Taherpour Khalil, Carević, Ivana, Yahyaei, Ahmad, "Neocomian Fahliyan formation carbonates in the oil well X2 (Dorood oil field, Persian Gulf): Biostratigraphic data from benthic foraminifera and algae" in Iranian Journal of Earth Sciences, 11, no. 3 (2019):173-182,
https://hdl.handle.net/21.15107/rcub_gery_1018 .

TY  - JOUR
AU  - Taherpour-Khalil-Abad, Morteza
AU  - Taheri, Jafar
AU  - Majidifard, Mahmoud Reza
AU  - Hassanzadeh, Zinat
AU  - Carević, Ivana
PY  - 2019
UR  - https://gery.gef.bg.ac.rs/handle/123456789/983
AB  - During micropaleontological investigations on the Lower Cretaceous successions of the Tirgan Formation in Kopet-Dagh sedimentary basin, some new achievements are yielded. In this regards, the first occurrence of Bispiraloconulus serbicus Schlagintweit, Bucur & Sudar in close association with Torremiroella hispanica Brun & Canérot is reported for the first time from the Upper Barremian of Kopet-Dagh sedimentary basin (NE Iran). The biostratigraphic investigations were carried out on a 197.5 m thick Gelian stratigraphic succession cropping out along the Tirgan Formation located 35 km southwest of Shirvan town. This study reviews the palaeogeographical distribution and age of Bispiraloconulus serbicus Schlagintweit, Bucur& Sudar and Torremiroella hispanica Brun & Canérot along the northern Tethyan margins and extends its palaeobiogeographical existence.
AB  - Mikropaleontološka istraživanja donjokredne sukcesije formacije Tirgan u Kopet-Dag sedimentacionom basenu (SI Iran) su pružila nove podatke. S tim u vezi, prvi put je u sedimentima Gornjeg Barema dokumentovan Bispiraloconulus serbicus Schlagintweit, Bucur& Sudar u asocijaciji sa Torremiroella hispanica Brun & Canérot. Biostratigrafska istraživanja su obavljena na stratigrafskom profilu Gelian (Formacija Tirgan) ukupne debljine 197,5 m koji je otkriven 35 km jugozapadno od grada Shirvan. U radu je data revizija paleogeografskog rasprostranjenja i starosti foraminifera Bispiraloconulus serbicus Schlagintweit, Bucur & Sudar i Torremiroella hispanica Brun & Canérot duž severnogo boda Tetisa.
PB  - Univerzitet u Beogradu - Rudarsko-geološki fakultet, Beograd
T2  - Geološki Anali Balkanskoga Poluostrva
T1  - Bispiraloconulus serbicus Schlagintweit, Bucur & Sudar, 2019 (arborescent benthic foraminifer) and Torremiroella hispanica Brun & Canérot, 1979 from the Late Barremian of Kopet-Dagh sedimentary basin (NE Iran) and their palaeobiogeographic revisions
T1  - Bispiraloconulus serbicus Schlagintweit, Bucur & Sudar, 2019 (arborescentni Bentoski foraminifer) i Torremiroella hispanica Brun & Canérot,1979 iz gornjobaremskog sedimentnog basena Kopet-Dag (SI Iran) i njihove paleobiogeografske revizije
VL  - 80
IS  - 2
SP  - 39
EP  - 51
DO  - 10.2298/GABP1902039T
UR  - https://hdl.handle.net/21.15107/rcub_gery_983
ER  - 

@article{
author = "Taherpour-Khalil-Abad, Morteza and Taheri, Jafar and Majidifard, Mahmoud Reza and Hassanzadeh, Zinat and Carević, Ivana",
year = "2019",
abstract = "During micropaleontological investigations on the Lower Cretaceous successions of the Tirgan Formation in Kopet-Dagh sedimentary basin, some new achievements are yielded. In this regards, the first occurrence of Bispiraloconulus serbicus Schlagintweit, Bucur & Sudar in close association with Torremiroella hispanica Brun & Canérot is reported for the first time from the Upper Barremian of Kopet-Dagh sedimentary basin (NE Iran). The biostratigraphic investigations were carried out on a 197.5 m thick Gelian stratigraphic succession cropping out along the Tirgan Formation located 35 km southwest of Shirvan town. This study reviews the palaeogeographical distribution and age of Bispiraloconulus serbicus Schlagintweit, Bucur& Sudar and Torremiroella hispanica Brun & Canérot along the northern Tethyan margins and extends its palaeobiogeographical existence., Mikropaleontološka istraživanja donjokredne sukcesije formacije Tirgan u Kopet-Dag sedimentacionom basenu (SI Iran) su pružila nove podatke. S tim u vezi, prvi put je u sedimentima Gornjeg Barema dokumentovan Bispiraloconulus serbicus Schlagintweit, Bucur& Sudar u asocijaciji sa Torremiroella hispanica Brun & Canérot. Biostratigrafska istraživanja su obavljena na stratigrafskom profilu Gelian (Formacija Tirgan) ukupne debljine 197,5 m koji je otkriven 35 km jugozapadno od grada Shirvan. U radu je data revizija paleogeografskog rasprostranjenja i starosti foraminifera Bispiraloconulus serbicus Schlagintweit, Bucur & Sudar i Torremiroella hispanica Brun & Canérot duž severnogo boda Tetisa.",
publisher = "Univerzitet u Beogradu - Rudarsko-geološki fakultet, Beograd",
journal = "Geološki Anali Balkanskoga Poluostrva",
title = "Bispiraloconulus serbicus Schlagintweit, Bucur & Sudar, 2019 (arborescent benthic foraminifer) and Torremiroella hispanica Brun & Canérot, 1979 from the Late Barremian of Kopet-Dagh sedimentary basin (NE Iran) and their palaeobiogeographic revisions, Bispiraloconulus serbicus Schlagintweit, Bucur & Sudar, 2019 (arborescentni Bentoski foraminifer) i Torremiroella hispanica Brun & Canérot,1979 iz gornjobaremskog sedimentnog basena Kopet-Dag (SI Iran) i njihove paleobiogeografske revizije",
volume = "80",
number = "2",
pages = "39-51",
doi = "10.2298/GABP1902039T",
url = "https://hdl.handle.net/21.15107/rcub_gery_983"
}

Taherpour-Khalil-Abad, M., Taheri, J., Majidifard, M. R., Hassanzadeh, Z.,& Carević, I.. (2019). Bispiraloconulus serbicus Schlagintweit, Bucur & Sudar, 2019 (arborescent benthic foraminifer) and Torremiroella hispanica Brun & Canérot, 1979 from the Late Barremian of Kopet-Dagh sedimentary basin (NE Iran) and their palaeobiogeographic revisions. in Geološki Anali Balkanskoga Poluostrva
Univerzitet u Beogradu - Rudarsko-geološki fakultet, Beograd., 80(2), 39-51.
https://doi.org/10.2298/GABP1902039T
https://hdl.handle.net/21.15107/rcub_gery_983

Taherpour-Khalil-Abad M, Taheri J, Majidifard MR, Hassanzadeh Z, Carević I. Bispiraloconulus serbicus Schlagintweit, Bucur & Sudar, 2019 (arborescent benthic foraminifer) and Torremiroella hispanica Brun & Canérot, 1979 from the Late Barremian of Kopet-Dagh sedimentary basin (NE Iran) and their palaeobiogeographic revisions. in Geološki Anali Balkanskoga Poluostrva. 2019;80(2):39-51.
doi:10.2298/GABP1902039T
https://hdl.handle.net/21.15107/rcub_gery_983 .

Taherpour-Khalil-Abad, Morteza, Taheri, Jafar, Majidifard, Mahmoud Reza, Hassanzadeh, Zinat, Carević, Ivana, "Bispiraloconulus serbicus Schlagintweit, Bucur & Sudar, 2019 (arborescent benthic foraminifer) and Torremiroella hispanica Brun & Canérot, 1979 from the Late Barremian of Kopet-Dagh sedimentary basin (NE Iran) and their palaeobiogeographic revisions" in Geološki Anali Balkanskoga Poluostrva, 80, no. 2 (2019):39-51,
https://doi.org/10.2298/GABP1902039T .,
https://hdl.handle.net/21.15107/rcub_gery_983 .

TY  - JOUR
AU  - Manojlović, Sanja
AU  - Antić, Marija
AU  - Šantić, Danica
AU  - Sibinović, Mikica
AU  - Carević, Ivana
AU  - Srejić, Tanja
PY  - 2018
UR  - https://gery.gef.bg.ac.rs/handle/123456789/947
AB  - In many Eastern European countries, the standard of living increased as a result of the process of industrialization in the second half of the 20th Century. Consequently, the population in rural areas with small-scale farming decreased due to the availability of employment elsewhere. This directly impacted soil erosion (and thereby sustainability of the land), but the degree and direction are not well known. This study investigates two municipalities within Serbia, their change in population and its impact on land use changes and soil erosion. The standard of living increased after the industrialization process in the 1960s within these municipalities. The erosion potential model is used to calculate gross annual erosion. The changes related to population and arable land in rural settlements are analyzed according to proportional spatial changes. The results show an overall decrease of erosion intensity in the study area. In addition, two basic findings are derived: first, the highest level of human impact on soil is in rural settlements at the lowest elevation zones, where erosion intensity shows the least amount of decrease; and, second, the most intensive depopulation process, recorded in higher elevation zones, indicates a rapid decrease of erosion intensity.
PB  - MDPI, Basel
T2  - Sustainability
T1  - Anthropogenic Impact on Erosion Intensity: Case Study of Rural Areas of Pirot and Dimitrovgrad Municipalities, Serbia
VL  - 10
IS  - 3
DO  - 10.3390/su10030826
UR  - https://hdl.handle.net/21.15107/rcub_gery_947
ER  - 

@article{
author = "Manojlović, Sanja and Antić, Marija and Šantić, Danica and Sibinović, Mikica and Carević, Ivana and Srejić, Tanja",
year = "2018",
abstract = "In many Eastern European countries, the standard of living increased as a result of the process of industrialization in the second half of the 20th Century. Consequently, the population in rural areas with small-scale farming decreased due to the availability of employment elsewhere. This directly impacted soil erosion (and thereby sustainability of the land), but the degree and direction are not well known. This study investigates two municipalities within Serbia, their change in population and its impact on land use changes and soil erosion. The standard of living increased after the industrialization process in the 1960s within these municipalities. The erosion potential model is used to calculate gross annual erosion. The changes related to population and arable land in rural settlements are analyzed according to proportional spatial changes. The results show an overall decrease of erosion intensity in the study area. In addition, two basic findings are derived: first, the highest level of human impact on soil is in rural settlements at the lowest elevation zones, where erosion intensity shows the least amount of decrease; and, second, the most intensive depopulation process, recorded in higher elevation zones, indicates a rapid decrease of erosion intensity.",
publisher = "MDPI, Basel",
journal = "Sustainability",
title = "Anthropogenic Impact on Erosion Intensity: Case Study of Rural Areas of Pirot and Dimitrovgrad Municipalities, Serbia",
volume = "10",
number = "3",
doi = "10.3390/su10030826",
url = "https://hdl.handle.net/21.15107/rcub_gery_947"
}

Manojlović, S., Antić, M., Šantić, D., Sibinović, M., Carević, I.,& Srejić, T.. (2018). Anthropogenic Impact on Erosion Intensity: Case Study of Rural Areas of Pirot and Dimitrovgrad Municipalities, Serbia. in Sustainability
MDPI, Basel., 10(3).
https://doi.org/10.3390/su10030826
https://hdl.handle.net/21.15107/rcub_gery_947

Manojlović S, Antić M, Šantić D, Sibinović M, Carević I, Srejić T. Anthropogenic Impact on Erosion Intensity: Case Study of Rural Areas of Pirot and Dimitrovgrad Municipalities, Serbia. in Sustainability. 2018;10(3).
doi:10.3390/su10030826
https://hdl.handle.net/21.15107/rcub_gery_947 .

Manojlović, Sanja, Antić, Marija, Šantić, Danica, Sibinović, Mikica, Carević, Ivana, Srejić, Tanja, "Anthropogenic Impact on Erosion Intensity: Case Study of Rural Areas of Pirot and Dimitrovgrad Municipalities, Serbia" in Sustainability, 10, no. 3 (2018),
https://doi.org/10.3390/su10030826 .,
https://hdl.handle.net/21.15107/rcub_gery_947 .

TY  - JOUR
AU  - Carević, Ivana
AU  - Taherpour-Khalil-Abad, Morteza
AU  - Mirković, Monika
AU  - Jovanović, Velimir
AU  - Mojtahedin, Elham
AU  - Vušković, Dragana
AU  - Vušković, Dragana
PY  - 2018
UR  - https://gery.gef.bg.ac.rs/handle/123456789/945
AB  - The occurrence of microfossil assemblage represented by calpionellids in close association with benthic foraminifera and encrusting Crescentiella morronensis is reported for the first time from the Upper Tithonian of NE Serbia. The biostratigraphic and sedimentological investigations were carried out on a 250 m thick carbonate succession in Jelenska Stena quarry cropping out along the Danube River Gorge in the border area of Serbian Carpatho-Balkanides and Romanian Southern Carphatians. On the basis of determined benthic foraminiferal taxa Textularia sp. cf. T bettenstaedti and Everticyclammina praekelleri in the lower part of the succession and calpionellid association dominated by the representatives of calpionellid genera Tintinnopsella, Crassicollaria and Calpionella the carbonate succession is assigned to the Upper Tithonian. The scarcity of calpionellid zonal species prevents the nominal zones being recognized. Petrographic analysis of thin-sections led to the recognition of three basin microfacies types: bioclastic wackestone, bioclastic peloidal wackestone/packstone and mudstone. These microfacies characterize the SMF 3 and SMF 4 which indicate deposition in slope and toe-of-slope environments. This study extends the palaeogeographical distribution of Upper Tithonian calpionellids along the northern Tethyan margins. The investigated carbonate succession is compared with coeval strata from other northern Tethyan regions.
PB  - Slovak Acad Sciences Geological  Inst, Bratislava
T2  - Geologica Carpathica
T1  - Calpionellid biostratigraphy and microfacies of the Upper Tithonian pelagic carbonates in northeastern Serbia (Carpatho-Balkanides)
VL  - 69
IS  - 3
SP  - 301
EP  - 311
DO  - 10.1515/geoca-2018-0018
UR  - https://hdl.handle.net/21.15107/rcub_gery_945
ER  - 

@article{
author = "Carević, Ivana and Taherpour-Khalil-Abad, Morteza and Mirković, Monika and Jovanović, Velimir and Mojtahedin, Elham and Vušković, Dragana and Vušković, Dragana",
year = "2018",
abstract = "The occurrence of microfossil assemblage represented by calpionellids in close association with benthic foraminifera and encrusting Crescentiella morronensis is reported for the first time from the Upper Tithonian of NE Serbia. The biostratigraphic and sedimentological investigations were carried out on a 250 m thick carbonate succession in Jelenska Stena quarry cropping out along the Danube River Gorge in the border area of Serbian Carpatho-Balkanides and Romanian Southern Carphatians. On the basis of determined benthic foraminiferal taxa Textularia sp. cf. T bettenstaedti and Everticyclammina praekelleri in the lower part of the succession and calpionellid association dominated by the representatives of calpionellid genera Tintinnopsella, Crassicollaria and Calpionella the carbonate succession is assigned to the Upper Tithonian. The scarcity of calpionellid zonal species prevents the nominal zones being recognized. Petrographic analysis of thin-sections led to the recognition of three basin microfacies types: bioclastic wackestone, bioclastic peloidal wackestone/packstone and mudstone. These microfacies characterize the SMF 3 and SMF 4 which indicate deposition in slope and toe-of-slope environments. This study extends the palaeogeographical distribution of Upper Tithonian calpionellids along the northern Tethyan margins. The investigated carbonate succession is compared with coeval strata from other northern Tethyan regions.",
publisher = "Slovak Acad Sciences Geological  Inst, Bratislava",
journal = "Geologica Carpathica",
title = "Calpionellid biostratigraphy and microfacies of the Upper Tithonian pelagic carbonates in northeastern Serbia (Carpatho-Balkanides)",
volume = "69",
number = "3",
pages = "301-311",
doi = "10.1515/geoca-2018-0018",
url = "https://hdl.handle.net/21.15107/rcub_gery_945"
}

Carević, I., Taherpour-Khalil-Abad, M., Mirković, M., Jovanović, V., Mojtahedin, E., Vušković, D.,& Vušković, D.. (2018). Calpionellid biostratigraphy and microfacies of the Upper Tithonian pelagic carbonates in northeastern Serbia (Carpatho-Balkanides). in Geologica Carpathica
Slovak Acad Sciences Geological  Inst, Bratislava., 69(3), 301-311.
https://doi.org/10.1515/geoca-2018-0018
https://hdl.handle.net/21.15107/rcub_gery_945

Carević I, Taherpour-Khalil-Abad M, Mirković M, Jovanović V, Mojtahedin E, Vušković D, Vušković D. Calpionellid biostratigraphy and microfacies of the Upper Tithonian pelagic carbonates in northeastern Serbia (Carpatho-Balkanides). in Geologica Carpathica. 2018;69(3):301-311.
doi:10.1515/geoca-2018-0018
https://hdl.handle.net/21.15107/rcub_gery_945 .

Carević, Ivana, Taherpour-Khalil-Abad, Morteza, Mirković, Monika, Jovanović, Velimir, Mojtahedin, Elham, Vušković, Dragana, Vušković, Dragana, "Calpionellid biostratigraphy and microfacies of the Upper Tithonian pelagic carbonates in northeastern Serbia (Carpatho-Balkanides)" in Geologica Carpathica, 69, no. 3 (2018):301-311,
https://doi.org/10.1515/geoca-2018-0018 .,
https://hdl.handle.net/21.15107/rcub_gery_945 .

TY  - JOUR
AU  - Rogan, Saša
AU  - Sentić, Milica
AU  - Vidović, Milka
AU  - Tanasijević, Gordana
AU  - Carević, Ivana
PY  - 2018
UR  - https://gery.gef.bg.ac.rs/handle/123456789/929
AB  - In the research phase of the geological status of the area of southeastern Banat, samples were collected from surface waters, wells, and lakes. The content of U, Ra, Rn is determined in water. The sampling network was adjusted to the hydrographic characteristics of the terrain, and a hydrogeochemical map has been made at a scale of 1:50 000. In addition to hydrogeochemical prospecting, samples of the soil river sediments were taken to determine the profile of the coast of the following lakes: Vračarevo, Šaransko, Bagersko and Veliko lake. The regional hydrogeochemical prospecting included the area of the Bela Crkva, which drained the sediments of Negotin and Kvartara. In this area and wider, in accordance with the results of regional investigation, semi-geological and semi-geochemical research was carried out to identify resources of mineral deposits as well as the sources for water supply of rural settlements. During research, samples of water from surface streams, sources, wells, lakes, water reservoirs, creek sediments and wall samples were collected and examined.
AB  - U fazi istraživanja geološkog statusa područja jugoistočnog Banata, prikupljeni su uzorci sa površinskih akvatorija, bunara i jezera. U vodi je determinisan sadržaj U, Ra, Rn. Mreža uzorkovanja je prilagođena hidrografskim karakteristikama terena, i napravljena je hidrogeohemijska mapa 1:50 000. Pored hidrogeohemijske prospekcije, uzeti su uzorci rečnih sedimenata zemljišta kako bi se odredio profil obale sledećih jezera: Vračarevo, Šaransko, Bagersko i Veliko jezero. Regionalna hidrogeohemijska prospekcija obuhvatila je područje Bele Crkve, koje dreniraju sedimente Neogena i Kvartara. U ovom području i šire, u skladu sa rezultatima regionalnih ispitivanja, obavljena su i poludetaljna geološka-geohemijska istraživanja u cilju identifikacije ležišta mineralnih sirovina, kao i izvorišta za vodosnabdevanje ruralnih naselja. U toku prospekcije, prikupljeni i ispitani su uzorci voda iz površinskih tokova, izvora, bunara, jezera, vodenih akumulacija, potočnih sedimenata i uzorci stena.
PB  - Udruženje za tehnologiju vode i sanitarno inžinjerstvo, Beograd
T2  - Voda i sanitarna tehnika
T1  - Hydrogeochemical Investigation of South-eastern Banat, a Part of Republic of Serbia
T1  - Hidrogeohemijska istraživanja u jugoistočnom Banatu na teritoriji Republike Srbije
VL  - 48
IS  - 1
SP  - 47
EP  - 53
UR  - https://hdl.handle.net/21.15107/rcub_gery_929
ER  - 

@article{
author = "Rogan, Saša and Sentić, Milica and Vidović, Milka and Tanasijević, Gordana and Carević, Ivana",
year = "2018",
abstract = "In the research phase of the geological status of the area of southeastern Banat, samples were collected from surface waters, wells, and lakes. The content of U, Ra, Rn is determined in water. The sampling network was adjusted to the hydrographic characteristics of the terrain, and a hydrogeochemical map has been made at a scale of 1:50 000. In addition to hydrogeochemical prospecting, samples of the soil river sediments were taken to determine the profile of the coast of the following lakes: Vračarevo, Šaransko, Bagersko and Veliko lake. The regional hydrogeochemical prospecting included the area of the Bela Crkva, which drained the sediments of Negotin and Kvartara. In this area and wider, in accordance with the results of regional investigation, semi-geological and semi-geochemical research was carried out to identify resources of mineral deposits as well as the sources for water supply of rural settlements. During research, samples of water from surface streams, sources, wells, lakes, water reservoirs, creek sediments and wall samples were collected and examined., U fazi istraživanja geološkog statusa područja jugoistočnog Banata, prikupljeni su uzorci sa površinskih akvatorija, bunara i jezera. U vodi je determinisan sadržaj U, Ra, Rn. Mreža uzorkovanja je prilagođena hidrografskim karakteristikama terena, i napravljena je hidrogeohemijska mapa 1:50 000. Pored hidrogeohemijske prospekcije, uzeti su uzorci rečnih sedimenata zemljišta kako bi se odredio profil obale sledećih jezera: Vračarevo, Šaransko, Bagersko i Veliko jezero. Regionalna hidrogeohemijska prospekcija obuhvatila je područje Bele Crkve, koje dreniraju sedimente Neogena i Kvartara. U ovom području i šire, u skladu sa rezultatima regionalnih ispitivanja, obavljena su i poludetaljna geološka-geohemijska istraživanja u cilju identifikacije ležišta mineralnih sirovina, kao i izvorišta za vodosnabdevanje ruralnih naselja. U toku prospekcije, prikupljeni i ispitani su uzorci voda iz površinskih tokova, izvora, bunara, jezera, vodenih akumulacija, potočnih sedimenata i uzorci stena.",
publisher = "Udruženje za tehnologiju vode i sanitarno inžinjerstvo, Beograd",
journal = "Voda i sanitarna tehnika",
title = "Hydrogeochemical Investigation of South-eastern Banat, a Part of Republic of Serbia, Hidrogeohemijska istraživanja u jugoistočnom Banatu na teritoriji Republike Srbije",
volume = "48",
number = "1",
pages = "47-53",
url = "https://hdl.handle.net/21.15107/rcub_gery_929"
}

Rogan, S., Sentić, M., Vidović, M., Tanasijević, G.,& Carević, I.. (2018). Hydrogeochemical Investigation of South-eastern Banat, a Part of Republic of Serbia. in Voda i sanitarna tehnika
Udruženje za tehnologiju vode i sanitarno inžinjerstvo, Beograd., 48(1), 47-53.
https://hdl.handle.net/21.15107/rcub_gery_929

Rogan S, Sentić M, Vidović M, Tanasijević G, Carević I. Hydrogeochemical Investigation of South-eastern Banat, a Part of Republic of Serbia. in Voda i sanitarna tehnika. 2018;48(1):47-53.
https://hdl.handle.net/21.15107/rcub_gery_929 .

Rogan, Saša, Sentić, Milica, Vidović, Milka, Tanasijević, Gordana, Carević, Ivana, "Hydrogeochemical Investigation of South-eastern Banat, a Part of Republic of Serbia" in Voda i sanitarna tehnika, 48, no. 1 (2018):47-53,
https://hdl.handle.net/21.15107/rcub_gery_929 .

TY  - CONF
AU  - Rogan, Saša
AU  - Gordanić, V.B.
AU  - Carević, Ivana
AU  - Sentić, Milica
PY  - 2018
UR  - https://gery.gef.bg.ac.rs/handle/123456789/910
AB  - Geochemical map of western and souther part of Serbia covers an area of about 30 000 km2 and also basins of rivers Ibar, Western Morava, Kolubara, Drina and Grand Morava. Representative samples from relevant profiles were collected according to WEGS (Western European Geochemical association). Samples were collected at the A-horizon at a depth of 15-20 cm from the ground surface; OB-overbank sediments at the depth of 80-100 cm and S-modern stream sediment. Geochemical mapping of lithological members was performed at 66 locations. The contents of natural radionuclides238 U,232 Th and40 K were analyzed. The results are shown on maps at a scale of 1: 1000000. Preserved geochemical record in the coastal profile of river flows will contribute to the assessment of anthropogenic impacts in the environment of rural settlements, particularly in the identification of geopathogenic zones of influence of natural radionuclides on human health. Research results have been shown on geochemical maps, diagrams and tables.
PB  - International Multidisciplinary Scientific Geoconference
C3  - International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Manage
T1  - Geochemical map 1:1.000.000 of western and southern part of Serbia with the ecological status
VL  - 18
IS  - 5.1
SP  - 431
EP  - 438
DO  - 10.5593/sgem2018/5.1/S20.056
UR  - https://hdl.handle.net/21.15107/rcub_gery_910
ER  - 

@conference{
author = "Rogan, Saša and Gordanić, V.B. and Carević, Ivana and Sentić, Milica",
year = "2018",
abstract = "Geochemical map of western and souther part of Serbia covers an area of about 30 000 km2 and also basins of rivers Ibar, Western Morava, Kolubara, Drina and Grand Morava. Representative samples from relevant profiles were collected according to WEGS (Western European Geochemical association). Samples were collected at the A-horizon at a depth of 15-20 cm from the ground surface; OB-overbank sediments at the depth of 80-100 cm and S-modern stream sediment. Geochemical mapping of lithological members was performed at 66 locations. The contents of natural radionuclides238 U,232 Th and40 K were analyzed. The results are shown on maps at a scale of 1: 1000000. Preserved geochemical record in the coastal profile of river flows will contribute to the assessment of anthropogenic impacts in the environment of rural settlements, particularly in the identification of geopathogenic zones of influence of natural radionuclides on human health. Research results have been shown on geochemical maps, diagrams and tables.",
publisher = "International Multidisciplinary Scientific Geoconference",
journal = "International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Manage",
title = "Geochemical map 1:1.000.000 of western and southern part of Serbia with the ecological status",
volume = "18",
number = "5.1",
pages = "431-438",
doi = "10.5593/sgem2018/5.1/S20.056",
url = "https://hdl.handle.net/21.15107/rcub_gery_910"
}

Rogan, S., Gordanić, V.B., Carević, I.,& Sentić, M.. (2018). Geochemical map 1:1.000.000 of western and southern part of Serbia with the ecological status. in International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Manage
International Multidisciplinary Scientific Geoconference., 18(5.1), 431-438.
https://doi.org/10.5593/sgem2018/5.1/S20.056
https://hdl.handle.net/21.15107/rcub_gery_910

Rogan S, Gordanić V, Carević I, Sentić M. Geochemical map 1:1.000.000 of western and southern part of Serbia with the ecological status. in International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Manage. 2018;18(5.1):431-438.
doi:10.5593/sgem2018/5.1/S20.056
https://hdl.handle.net/21.15107/rcub_gery_910 .

Rogan, Saša, Gordanić, V.B., Carević, Ivana, Sentić, Milica, "Geochemical map 1:1.000.000 of western and southern part of Serbia with the ecological status" in International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Manage, 18, no. 5.1 (2018):431-438,
https://doi.org/10.5593/sgem2018/5.1/S20.056 .,
https://hdl.handle.net/21.15107/rcub_gery_910 .

TY  - CONF
AU  - Rogan, Saša
AU  - Petrović, Vladimir
AU  - Carević, Ivana
AU  - Sentić, Milica
PY  - 2018
UR  - https://gery.gef.bg.ac.rs/handle/123456789/909
AB  - The explored area of Banat, located in NE Serbia, with its geological and geothermal characteristics, represents an area with extraordinary ecological potential. The geological structure of Banat is represented by various complexes of Neogene and Quaternary deposits. The Neogene sediments are mostly composed of sandstone, shale, marlstone, sand and gravel. Mesozoic igneous complex is represented by dacites, andesites and basalts. During Quaternary a relatively thick succession of genetically different types of sediments was deposited. Pleistocene and Holocene aeolian sand and loess and fluvial sandy-clayey alevrites, clays, sands and gravel cover the large area. Thickness and lithological composition of crust and lithosphere, as well as character, types and age of tectonic movements and magmatism decisively influence the content of radioactive elements (uranium, thorium and potassium) in the rocks. Nevertheless, the geothermal characteristics of a particular area are influenced in a significant extent by seismicity and hydrogeological properties. The small thickness of the crust and lithosphere, as a result of various geodynamic movements, during the lower and middle Miocene, classify the Pannonian Basin, and therefore the Banat area, among the most promising geothermal areas in Europe. The favorable geothermal characteristics of Banat also show high average values of geothermal gradient and terrestrial heat flux.
PB  - International Multidisciplinary Scientific Geoconference
C3  - International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Manage
T1  - Ekological aspect of the geothermal potentials of ne Serbia
VL  - 18
IS  - 5.1
SP  - 297
EP  - 304
DO  - 10.5593/sgem2018/5.1/S20.039
UR  - https://hdl.handle.net/21.15107/rcub_gery_909
ER  - 

@conference{
author = "Rogan, Saša and Petrović, Vladimir and Carević, Ivana and Sentić, Milica",
year = "2018",
abstract = "The explored area of Banat, located in NE Serbia, with its geological and geothermal characteristics, represents an area with extraordinary ecological potential. The geological structure of Banat is represented by various complexes of Neogene and Quaternary deposits. The Neogene sediments are mostly composed of sandstone, shale, marlstone, sand and gravel. Mesozoic igneous complex is represented by dacites, andesites and basalts. During Quaternary a relatively thick succession of genetically different types of sediments was deposited. Pleistocene and Holocene aeolian sand and loess and fluvial sandy-clayey alevrites, clays, sands and gravel cover the large area. Thickness and lithological composition of crust and lithosphere, as well as character, types and age of tectonic movements and magmatism decisively influence the content of radioactive elements (uranium, thorium and potassium) in the rocks. Nevertheless, the geothermal characteristics of a particular area are influenced in a significant extent by seismicity and hydrogeological properties. The small thickness of the crust and lithosphere, as a result of various geodynamic movements, during the lower and middle Miocene, classify the Pannonian Basin, and therefore the Banat area, among the most promising geothermal areas in Europe. The favorable geothermal characteristics of Banat also show high average values of geothermal gradient and terrestrial heat flux.",
publisher = "International Multidisciplinary Scientific Geoconference",
journal = "International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Manage",
title = "Ekological aspect of the geothermal potentials of ne Serbia",
volume = "18",
number = "5.1",
pages = "297-304",
doi = "10.5593/sgem2018/5.1/S20.039",
url = "https://hdl.handle.net/21.15107/rcub_gery_909"
}

Rogan, S., Petrović, V., Carević, I.,& Sentić, M.. (2018). Ekological aspect of the geothermal potentials of ne Serbia. in International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Manage
International Multidisciplinary Scientific Geoconference., 18(5.1), 297-304.
https://doi.org/10.5593/sgem2018/5.1/S20.039
https://hdl.handle.net/21.15107/rcub_gery_909

Rogan S, Petrović V, Carević I, Sentić M. Ekological aspect of the geothermal potentials of ne Serbia. in International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Manage. 2018;18(5.1):297-304.
doi:10.5593/sgem2018/5.1/S20.039
https://hdl.handle.net/21.15107/rcub_gery_909 .

Rogan, Saša, Petrović, Vladimir, Carević, Ivana, Sentić, Milica, "Ekological aspect of the geothermal potentials of ne Serbia" in International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Manage, 18, no. 5.1 (2018):297-304,
https://doi.org/10.5593/sgem2018/5.1/S20.039 .,
https://hdl.handle.net/21.15107/rcub_gery_909 .

TY  - JOUR
AU  - Rostami, Leila
AU  - Vaziri, Seyed Hamid
AU  - Jahani, Davood
AU  - Solgi, Ali
AU  - Taherpour-Khalil-Abad, Morteza
AU  - Carević, Ivana
AU  - Yahyaei, Ahmad
PY  - 2018
UR  - https://gery.gef.bg.ac.rs/handle/123456789/897
AB  - The Dorood oilfield is located offshore in the northern part of the Persian Gulf. It partly underlies the Kharg Island. The Neocomian Fahliyan Formation represents the high-quality reservoir in the oilfield. It includes five carbonate members: The Manifa, Middle and Upper Yamama, Khami and Lower Ratawi. The Fahliyan Formation in the studied well attains a thickness of 378.1 m and mainly consists of thin-bedded limestones. It unconformably overlies the evaporate Hith Formation and conformably underlies the Gadvan Formation. An integrated biostratigraphic (benthic foraminifera and algae) and lithostratigraphic study is presented. Paleontological studies led to the identification of 19 genera and 29 species of benthic foraminifera and 10 genera and 9 species of calcareous algae. Two biozones of Berriasian through Valanginian age have been recognized. These are Lithocodium aggregatum-Salpingoporella muehlbergii assemblage zone (Valanginian) and Pseudocyclammina lituus- Coscinoconus assemblage zone (Berriasian-Valanginian).
PB  - Univ Tehran, Tehran
T2  - Geopersia
T1  - Benthic foraminiferal and calcareous algal biostratigraphy of the Fahliyan Formation in oil well X1, Dorood Oilfield, Persian Gulf
VL  - 8
IS  - 2
SP  - 319
EP  - 329
DO  - 10.22059/GEOPE.2018.256557.648385
UR  - https://hdl.handle.net/21.15107/rcub_gery_897
ER  - 

@article{
author = "Rostami, Leila and Vaziri, Seyed Hamid and Jahani, Davood and Solgi, Ali and Taherpour-Khalil-Abad, Morteza and Carević, Ivana and Yahyaei, Ahmad",
year = "2018",
abstract = "The Dorood oilfield is located offshore in the northern part of the Persian Gulf. It partly underlies the Kharg Island. The Neocomian Fahliyan Formation represents the high-quality reservoir in the oilfield. It includes five carbonate members: The Manifa, Middle and Upper Yamama, Khami and Lower Ratawi. The Fahliyan Formation in the studied well attains a thickness of 378.1 m and mainly consists of thin-bedded limestones. It unconformably overlies the evaporate Hith Formation and conformably underlies the Gadvan Formation. An integrated biostratigraphic (benthic foraminifera and algae) and lithostratigraphic study is presented. Paleontological studies led to the identification of 19 genera and 29 species of benthic foraminifera and 10 genera and 9 species of calcareous algae. Two biozones of Berriasian through Valanginian age have been recognized. These are Lithocodium aggregatum-Salpingoporella muehlbergii assemblage zone (Valanginian) and Pseudocyclammina lituus- Coscinoconus assemblage zone (Berriasian-Valanginian).",
publisher = "Univ Tehran, Tehran",
journal = "Geopersia",
title = "Benthic foraminiferal and calcareous algal biostratigraphy of the Fahliyan Formation in oil well X1, Dorood Oilfield, Persian Gulf",
volume = "8",
number = "2",
pages = "319-329",
doi = "10.22059/GEOPE.2018.256557.648385",
url = "https://hdl.handle.net/21.15107/rcub_gery_897"
}

Rostami, L., Vaziri, S. H., Jahani, D., Solgi, A., Taherpour-Khalil-Abad, M., Carević, I.,& Yahyaei, A.. (2018). Benthic foraminiferal and calcareous algal biostratigraphy of the Fahliyan Formation in oil well X1, Dorood Oilfield, Persian Gulf. in Geopersia
Univ Tehran, Tehran., 8(2), 319-329.
https://doi.org/10.22059/GEOPE.2018.256557.648385
https://hdl.handle.net/21.15107/rcub_gery_897

Rostami L, Vaziri SH, Jahani D, Solgi A, Taherpour-Khalil-Abad M, Carević I, Yahyaei A. Benthic foraminiferal and calcareous algal biostratigraphy of the Fahliyan Formation in oil well X1, Dorood Oilfield, Persian Gulf. in Geopersia. 2018;8(2):319-329.
doi:10.22059/GEOPE.2018.256557.648385
https://hdl.handle.net/21.15107/rcub_gery_897 .

Rostami, Leila, Vaziri, Seyed Hamid, Jahani, Davood, Solgi, Ali, Taherpour-Khalil-Abad, Morteza, Carević, Ivana, Yahyaei, Ahmad, "Benthic foraminiferal and calcareous algal biostratigraphy of the Fahliyan Formation in oil well X1, Dorood Oilfield, Persian Gulf" in Geopersia, 8, no. 2 (2018):319-329,
https://doi.org/10.22059/GEOPE.2018.256557.648385 .,
https://hdl.handle.net/21.15107/rcub_gery_897 .

TY  - JOUR
AU  - Jovanović, Velimir
AU  - Carević, Ivana
PY  - 2016
UR  - https://gery.gef.bg.ac.rs/handle/123456789/792
AB  - Geological building materials that include building stones (structural and dimension stone), stones used to produce construction materials (binders, thermal insulation) and industrial stones are among the more important natural or, more specifically, geological resources. Their use is mostly related to construction, but also to certain other industries. When an area abounds in these resources, this can significantly boost its development, provided that the resources are used in a sus­tainable manner. This article discusses the possibilities of the Šumadija District.
AB  - Geološki građevinski materijali kao što su građevinski kamen (tehnički i arhitektonski), kamen za proizvodnju građevinskih materijala (ve­ziva, termoizolacioni materijali) i kamen u industriji, predstavlјaju jedan od važnih prirodnih, odnosno geoloških resursa. Nјihova eksploatacija, ve­zana je, pre svega za građevinsku delatnost, ali i za neke druge privredne grane. Bogatstvo u ovim resursima može značajno da doprinese lokalnom privrednom razvoju, uz uslov da se poštuju principi njihovog održivog korišćenja. Pri­mer koji je ovde prikazan odnosi se na teritoriju šumadijskog upravnog okruga.
PB  - Univerzitet u Beogradu - Geografski fakultet, Beograd
T2  - Zbornik radova - Geografski fakultet Univerziteta u Beogradu
T1  - Geological building materials as a factor with potential for development of the Šumadija District
T1  - Geološki građevinski materijali kao mogući faktor razvoja Šumadijskog okruga
IS  - 64
SP  - 517
EP  - 542
DO  - 10.5937/zrgfub1664517J
UR  - https://hdl.handle.net/21.15107/rcub_gery_792
ER  - 

@article{
author = "Jovanović, Velimir and Carević, Ivana",
year = "2016",
abstract = "Geological building materials that include building stones (structural and dimension stone), stones used to produce construction materials (binders, thermal insulation) and industrial stones are among the more important natural or, more specifically, geological resources. Their use is mostly related to construction, but also to certain other industries. When an area abounds in these resources, this can significantly boost its development, provided that the resources are used in a sus­tainable manner. This article discusses the possibilities of the Šumadija District., Geološki građevinski materijali kao što su građevinski kamen (tehnički i arhitektonski), kamen za proizvodnju građevinskih materijala (ve­ziva, termoizolacioni materijali) i kamen u industriji, predstavlјaju jedan od važnih prirodnih, odnosno geoloških resursa. Nјihova eksploatacija, ve­zana je, pre svega za građevinsku delatnost, ali i za neke druge privredne grane. Bogatstvo u ovim resursima može značajno da doprinese lokalnom privrednom razvoju, uz uslov da se poštuju principi njihovog održivog korišćenja. Pri­mer koji je ovde prikazan odnosi se na teritoriju šumadijskog upravnog okruga.",
publisher = "Univerzitet u Beogradu - Geografski fakultet, Beograd",
journal = "Zbornik radova - Geografski fakultet Univerziteta u Beogradu",
title = "Geological building materials as a factor with potential for development of the Šumadija District, Geološki građevinski materijali kao mogući faktor razvoja Šumadijskog okruga",
number = "64",
pages = "517-542",
doi = "10.5937/zrgfub1664517J",
url = "https://hdl.handle.net/21.15107/rcub_gery_792"
}

Jovanović, V.,& Carević, I.. (2016). Geological building materials as a factor with potential for development of the Šumadija District. in Zbornik radova - Geografski fakultet Univerziteta u Beogradu
Univerzitet u Beogradu - Geografski fakultet, Beograd.(64), 517-542.
https://doi.org/10.5937/zrgfub1664517J
https://hdl.handle.net/21.15107/rcub_gery_792

Jovanović V, Carević I. Geological building materials as a factor with potential for development of the Šumadija District. in Zbornik radova - Geografski fakultet Univerziteta u Beogradu. 2016;(64):517-542.
doi:10.5937/zrgfub1664517J
https://hdl.handle.net/21.15107/rcub_gery_792 .

Jovanović, Velimir, Carević, Ivana, "Geological building materials as a factor with potential for development of the Šumadija District" in Zbornik radova - Geografski fakultet Univerziteta u Beogradu, no. 64 (2016):517-542,
https://doi.org/10.5937/zrgfub1664517J .,
https://hdl.handle.net/21.15107/rcub_gery_792 .

TY  - JOUR
AU  - Petrović, Aleksandar S.
AU  - Carević, Ivana
PY  - 2015
UR  - https://gery.gef.bg.ac.rs/handle/123456789/670
AB  - The paper deals with the description of Samar natural bridge and collapse valley of Ravna River in eastern Serbia aiming to suggest an interpretation of their origin and development, in relationship with lithological and tectonic conditions, karst processes, and petrological analyses. In this study we present the geological setting, detailed morphology and hypothesis on the genesis of these karst landforms. The relationship between surface karst development and the geology is considerably acknowledged. The major contribution of the paper is to propose a framework for considering how recrystallization of limestone can affect the weathering potential of karst landforms and to introduce a term collapse valley. Finally, this study shows that the weathering potencial of the Samar natural bridge is decreased concerning the diagenetic changes these limestones underwent.
PB  - Zalozba Z R C
T2  - Acta Carsologica
T1  - Geological influence on the formation of samar natural bridge and collapse valley of ravna river from the ne kucaj mountains (carpatho-balkanides, eastern Serbia)
VL  - 44
IS  - 1
SP  - 37
EP  - 46
DO  - 10.3986/ac.v44i1.898
UR  - https://hdl.handle.net/21.15107/rcub_gery_670
ER  - 

@article{
author = "Petrović, Aleksandar S. and Carević, Ivana",
year = "2015",
abstract = "The paper deals with the description of Samar natural bridge and collapse valley of Ravna River in eastern Serbia aiming to suggest an interpretation of their origin and development, in relationship with lithological and tectonic conditions, karst processes, and petrological analyses. In this study we present the geological setting, detailed morphology and hypothesis on the genesis of these karst landforms. The relationship between surface karst development and the geology is considerably acknowledged. The major contribution of the paper is to propose a framework for considering how recrystallization of limestone can affect the weathering potential of karst landforms and to introduce a term collapse valley. Finally, this study shows that the weathering potencial of the Samar natural bridge is decreased concerning the diagenetic changes these limestones underwent.",
publisher = "Zalozba Z R C",
journal = "Acta Carsologica",
title = "Geological influence on the formation of samar natural bridge and collapse valley of ravna river from the ne kucaj mountains (carpatho-balkanides, eastern Serbia)",
volume = "44",
number = "1",
pages = "37-46",
doi = "10.3986/ac.v44i1.898",
url = "https://hdl.handle.net/21.15107/rcub_gery_670"
}

Petrović, A. S.,& Carević, I.. (2015). Geological influence on the formation of samar natural bridge and collapse valley of ravna river from the ne kucaj mountains (carpatho-balkanides, eastern Serbia). in Acta Carsologica
Zalozba Z R C., 44(1), 37-46.
https://doi.org/10.3986/ac.v44i1.898
https://hdl.handle.net/21.15107/rcub_gery_670

Petrović AS, Carević I. Geological influence on the formation of samar natural bridge and collapse valley of ravna river from the ne kucaj mountains (carpatho-balkanides, eastern Serbia). in Acta Carsologica. 2015;44(1):37-46.
doi:10.3986/ac.v44i1.898
https://hdl.handle.net/21.15107/rcub_gery_670 .

Petrović, Aleksandar S., Carević, Ivana, "Geological influence on the formation of samar natural bridge and collapse valley of ravna river from the ne kucaj mountains (carpatho-balkanides, eastern Serbia)" in Acta Carsologica, 44, no. 1 (2015):37-46,
https://doi.org/10.3986/ac.v44i1.898 .,
https://hdl.handle.net/21.15107/rcub_gery_670 .

TY  - JOUR
AU  - Vušković, Dragana
AU  - Carević, Ivana
AU  - Jovanović, Velimir
AU  - Biočanin, Nataša
PY  - 2014
UR  - https://gery.gef.bg.ac.rs/handle/123456789/608
PB  - Srpsko geografsko društvo, Beograd
T2  - Glasnik Srpskog geografskog društva
T1  - Analysis of ground water quality in terms of geological setting in the territory of the Mesić village for the purpose of bottling (municipality of Vršac)
VL  - 94
IS  - 4
SP  - 91
EP  - 108
DO  - 10.2298/GSGD1404091V
UR  - https://hdl.handle.net/21.15107/rcub_gery_608
ER  - 

@article{
author = "Vušković, Dragana and Carević, Ivana and Jovanović, Velimir and Biočanin, Nataša",
year = "2014",
publisher = "Srpsko geografsko društvo, Beograd",
journal = "Glasnik Srpskog geografskog društva",
title = "Analysis of ground water quality in terms of geological setting in the territory of the Mesić village for the purpose of bottling (municipality of Vršac)",
volume = "94",
number = "4",
pages = "91-108",
doi = "10.2298/GSGD1404091V",
url = "https://hdl.handle.net/21.15107/rcub_gery_608"
}

Vušković, D., Carević, I., Jovanović, V.,& Biočanin, N.. (2014). Analysis of ground water quality in terms of geological setting in the territory of the Mesić village for the purpose of bottling (municipality of Vršac). in Glasnik Srpskog geografskog društva
Srpsko geografsko društvo, Beograd., 94(4), 91-108.
https://doi.org/10.2298/GSGD1404091V
https://hdl.handle.net/21.15107/rcub_gery_608

Vušković D, Carević I, Jovanović V, Biočanin N. Analysis of ground water quality in terms of geological setting in the territory of the Mesić village for the purpose of bottling (municipality of Vršac). in Glasnik Srpskog geografskog društva. 2014;94(4):91-108.
doi:10.2298/GSGD1404091V
https://hdl.handle.net/21.15107/rcub_gery_608 .

Vušković, Dragana, Carević, Ivana, Jovanović, Velimir, Biočanin, Nataša, "Analysis of ground water quality in terms of geological setting in the territory of the Mesić village for the purpose of bottling (municipality of Vršac)" in Glasnik Srpskog geografskog društva, 94, no. 4 (2014):91-108,
https://doi.org/10.2298/GSGD1404091V .,
https://hdl.handle.net/21.15107/rcub_gery_608 .

TY  - JOUR
AU  - Carević, Ivana
AU  - Abad, Morteza Taherpour Khalil
AU  - Ljubović-Obradović, Darivojka
AU  - Vaziri, Seyed Hamid
AU  - Mirković, Monika
AU  - Aryaei, Ali Asghar
AU  - Stejić, Petar
AU  - Ashouri, Ali Reza
PY  - 2013
UR  - https://gery.gef.bg.ac.rs/handle/123456789/598
AB  - In the Getic of the Carpatho-Balcanides (eastern Serbia) and the Tirgan Formation of the Kopet-Dagh Basin (northeast Iran), platform carbonates were deposited during the Barremian/Early Aptian in environments in the domain of the northern Alpine Tethys and deformed during the Alpine orogeny. In this study, Urgonian carbonate platform deposits are discussed in detail with regard to depositional facies, microfacies, biostratigraphy, palaeoenvironments and palaeoecology. Detailed sedimentological and palaeontological investigations have been carried out on five sections in eastern Serbia and three sections in northeast Iran supported by an analysis of 392 thin-sections. Petrographic analysis of thin-sections led to the recognition of eight microfacies types grouped into four facies zones. A supratidal-intertidal (restricted)-intertidal (open-lagoon)-platform-margin sand-shoal transition was recorded in both areas. Supratidal facies are characterized by bioclastic mudstones and fenestral and peloidal wackestones and packstones; intertidal (restricted) facies are represented by bioclastic wackestones, whereas intertidal (open-lagoon) facies are indicated by bioclastic packstones/grainstones and oncoid grainstones. High-energy sand-shoal fades are dominated by ooid grainstones/rudstones followed by orbitolinid packstones. Benthic foraminifera are especially abundant and along with calcareous algae are the most important fossils used for age determination of shallow-marine carbonate deposits. Thirty-two benthic foraminiferal genera were identified from eastern Serbia with an additional 38 genera from northeast Iran dominated by agglutinated forms. Identified calcareous algae provide significant data for depositional environments and palaeoecology. The microfossil associations in the two regions are very similar and share a number of common characteristics, but also some differences and show a strong affinity to those of the northern margins of Tethys. In both study areas shallow-marine environments of the Barremian/Early Aptian were replaced by deep-marine conditions during the Late Cretaceous. (C) 2012 Elsevier Ltd. All rights reserved.
PB  - Academic Press Ltd- Elsevier Science Ltd, London
T2  - Cretaceous Research
T1  - Comparisons between the Urgonian platform carbonates from eastern Serbia (Carpatho-Balkanides) and northeast Iran (Kopet-Dagh Basin): Depositional facies, microfacies, biostratigraphy, palaeoenvironments and palaeoecology
VL  - 40
SP  - 110
EP  - 130
DO  - 10.1016/j.cretres.2012.06.003
UR  - https://hdl.handle.net/21.15107/rcub_gery_598
ER  - 

@article{
author = "Carević, Ivana and Abad, Morteza Taherpour Khalil and Ljubović-Obradović, Darivojka and Vaziri, Seyed Hamid and Mirković, Monika and Aryaei, Ali Asghar and Stejić, Petar and Ashouri, Ali Reza",
year = "2013",
abstract = "In the Getic of the Carpatho-Balcanides (eastern Serbia) and the Tirgan Formation of the Kopet-Dagh Basin (northeast Iran), platform carbonates were deposited during the Barremian/Early Aptian in environments in the domain of the northern Alpine Tethys and deformed during the Alpine orogeny. In this study, Urgonian carbonate platform deposits are discussed in detail with regard to depositional facies, microfacies, biostratigraphy, palaeoenvironments and palaeoecology. Detailed sedimentological and palaeontological investigations have been carried out on five sections in eastern Serbia and three sections in northeast Iran supported by an analysis of 392 thin-sections. Petrographic analysis of thin-sections led to the recognition of eight microfacies types grouped into four facies zones. A supratidal-intertidal (restricted)-intertidal (open-lagoon)-platform-margin sand-shoal transition was recorded in both areas. Supratidal facies are characterized by bioclastic mudstones and fenestral and peloidal wackestones and packstones; intertidal (restricted) facies are represented by bioclastic wackestones, whereas intertidal (open-lagoon) facies are indicated by bioclastic packstones/grainstones and oncoid grainstones. High-energy sand-shoal fades are dominated by ooid grainstones/rudstones followed by orbitolinid packstones. Benthic foraminifera are especially abundant and along with calcareous algae are the most important fossils used for age determination of shallow-marine carbonate deposits. Thirty-two benthic foraminiferal genera were identified from eastern Serbia with an additional 38 genera from northeast Iran dominated by agglutinated forms. Identified calcareous algae provide significant data for depositional environments and palaeoecology. The microfossil associations in the two regions are very similar and share a number of common characteristics, but also some differences and show a strong affinity to those of the northern margins of Tethys. In both study areas shallow-marine environments of the Barremian/Early Aptian were replaced by deep-marine conditions during the Late Cretaceous. (C) 2012 Elsevier Ltd. All rights reserved.",
publisher = "Academic Press Ltd- Elsevier Science Ltd, London",
journal = "Cretaceous Research",
title = "Comparisons between the Urgonian platform carbonates from eastern Serbia (Carpatho-Balkanides) and northeast Iran (Kopet-Dagh Basin): Depositional facies, microfacies, biostratigraphy, palaeoenvironments and palaeoecology",
volume = "40",
pages = "110-130",
doi = "10.1016/j.cretres.2012.06.003",
url = "https://hdl.handle.net/21.15107/rcub_gery_598"
}

Carević, I., Abad, M. T. K., Ljubović-Obradović, D., Vaziri, S. H., Mirković, M., Aryaei, A. A., Stejić, P.,& Ashouri, A. R.. (2013). Comparisons between the Urgonian platform carbonates from eastern Serbia (Carpatho-Balkanides) and northeast Iran (Kopet-Dagh Basin): Depositional facies, microfacies, biostratigraphy, palaeoenvironments and palaeoecology. in Cretaceous Research
Academic Press Ltd- Elsevier Science Ltd, London., 40, 110-130.
https://doi.org/10.1016/j.cretres.2012.06.003
https://hdl.handle.net/21.15107/rcub_gery_598

Carević I, Abad MTK, Ljubović-Obradović D, Vaziri SH, Mirković M, Aryaei AA, Stejić P, Ashouri AR. Comparisons between the Urgonian platform carbonates from eastern Serbia (Carpatho-Balkanides) and northeast Iran (Kopet-Dagh Basin): Depositional facies, microfacies, biostratigraphy, palaeoenvironments and palaeoecology. in Cretaceous Research. 2013;40:110-130.
doi:10.1016/j.cretres.2012.06.003
https://hdl.handle.net/21.15107/rcub_gery_598 .

Carević, Ivana, Abad, Morteza Taherpour Khalil, Ljubović-Obradović, Darivojka, Vaziri, Seyed Hamid, Mirković, Monika, Aryaei, Ali Asghar, Stejić, Petar, Ashouri, Ali Reza, "Comparisons between the Urgonian platform carbonates from eastern Serbia (Carpatho-Balkanides) and northeast Iran (Kopet-Dagh Basin): Depositional facies, microfacies, biostratigraphy, palaeoenvironments and palaeoecology" in Cretaceous Research, 40 (2013):110-130,
https://doi.org/10.1016/j.cretres.2012.06.003 .,
https://hdl.handle.net/21.15107/rcub_gery_598 .

TY  - JOUR
AU  - Dragićević, Slavoljub
AU  - Carević, Ivana
AU  - Kostadinov, Stanimir
AU  - Novković, Ivan
AU  - Abolmasov, Biljana
AU  - Milojković, Boban
AU  - Simić, Dušan
PY  - 2012
UR  - https://gery.gef.bg.ac.rs/handle/123456789/482
AB  - According to estimates, 25% of the territory of the Republic of Serbia is affected by landslide processes. In the spring, when snowmelt is accompanied by the maximum amount of precipitation, a great number of landslides have been activated within the territory of Serbia. The year 2006 had a particularly large number of registered landslides accompanied by huge material damages. Because a landslide data base for the territory of Serbia does not exist, it is very difficult to carry out the regular assignment of land use and to make a spatial development strategy. This imposed a need for methodological development of landslide hazard zonation (LHZ) for the territory of Serbia. The Kolubara River Basin was selected as an area with a significant number of landslides occurence. The spatial distribution of landslides is a result of the interaction of many parameters. Landslide susceptibility zones in the Kolubara River basin were identified by heuristic analysis of landslide causal factors - local topography, morphological and geological setting, and the existing and past landslides identified the study area. Based on the results obtained in this study, it was found that 243.75 km(2) or 6.69% of the total area was prone to landsliding. The results can be implemented as a base for development of LHZ model for the overall territory of Serbia, and will represent the first step for compilation of a landslide data base.
PB  - North Univ  Baia Mare
T2  - Carpathian Journal of Earth and Environmental Sciences
T1  - Landslide susceptibility zonation in the Kolubara river basin (western Serbia) - analysis of input data
VL  - 7
IS  - 2
SP  - 37
EP  - 47
UR  - https://hdl.handle.net/21.15107/rcub_jakov_495
ER  - 

@article{
author = "Dragićević, Slavoljub and Carević, Ivana and Kostadinov, Stanimir and Novković, Ivan and Abolmasov, Biljana and Milojković, Boban and Simić, Dušan",
year = "2012",
abstract = "According to estimates, 25% of the territory of the Republic of Serbia is affected by landslide processes. In the spring, when snowmelt is accompanied by the maximum amount of precipitation, a great number of landslides have been activated within the territory of Serbia. The year 2006 had a particularly large number of registered landslides accompanied by huge material damages. Because a landslide data base for the territory of Serbia does not exist, it is very difficult to carry out the regular assignment of land use and to make a spatial development strategy. This imposed a need for methodological development of landslide hazard zonation (LHZ) for the territory of Serbia. The Kolubara River Basin was selected as an area with a significant number of landslides occurence. The spatial distribution of landslides is a result of the interaction of many parameters. Landslide susceptibility zones in the Kolubara River basin were identified by heuristic analysis of landslide causal factors - local topography, morphological and geological setting, and the existing and past landslides identified the study area. Based on the results obtained in this study, it was found that 243.75 km(2) or 6.69% of the total area was prone to landsliding. The results can be implemented as a base for development of LHZ model for the overall territory of Serbia, and will represent the first step for compilation of a landslide data base.",
publisher = "North Univ  Baia Mare",
journal = "Carpathian Journal of Earth and Environmental Sciences",
title = "Landslide susceptibility zonation in the Kolubara river basin (western Serbia) - analysis of input data",
volume = "7",
number = "2",
pages = "37-47",
url = "https://hdl.handle.net/21.15107/rcub_jakov_495"
}

Dragićević, S., Carević, I., Kostadinov, S., Novković, I., Abolmasov, B., Milojković, B.,& Simić, D.. (2012). Landslide susceptibility zonation in the Kolubara river basin (western Serbia) - analysis of input data. in Carpathian Journal of Earth and Environmental Sciences
North Univ  Baia Mare., 7(2), 37-47.
https://hdl.handle.net/21.15107/rcub_jakov_495

Dragićević S, Carević I, Kostadinov S, Novković I, Abolmasov B, Milojković B, Simić D. Landslide susceptibility zonation in the Kolubara river basin (western Serbia) - analysis of input data. in Carpathian Journal of Earth and Environmental Sciences. 2012;7(2):37-47.
https://hdl.handle.net/21.15107/rcub_jakov_495 .

Dragićević, Slavoljub, Carević, Ivana, Kostadinov, Stanimir, Novković, Ivan, Abolmasov, Biljana, Milojković, Boban, Simić, Dušan, "Landslide susceptibility zonation in the Kolubara river basin (western Serbia) - analysis of input data" in Carpathian Journal of Earth and Environmental Sciences, 7, no. 2 (2012):37-47,
https://hdl.handle.net/21.15107/rcub_jakov_495 .

TY  - JOUR
AU  - Jovanović, Velimir
AU  - Carević, Ivana
AU  - Vušković, Dragana
AU  - Abad, Morteza Taherpour Khalil
PY  - 2012
UR  - https://gery.gef.bg.ac.rs/handle/123456789/500
AB  - Stratigraphic/palaeontological geosites of Stara Planina Mountain in east Serbia are well developed in the area of Serbian/Bulgarian state border, where with this occassion, three sections of exeptional geological and scientific interest are selected: Jelovica, Rosomač and Senokos. These geosites represent the important localities for study of Triassic and Jurassic terrigene-carbonate deposits, for which the scientific value from the domains of palaeontology, stratigraphy and sedimentology is widely known. The aim of this work is to represent the main scientific arguments for inventory and protection of detached transborder geological sites that are unique according to their composition and content.
AB  - Stratigrafsko-paleontološki geoobjekti Stare planine istočne Srbije su dobro razvijeni na području srpsko-bugarske državne granice gde su ovom prilikom izdvojena tri profila od izuzetnog geološkog i naučnog značaja: Jelovica, Rosomač i Senokos. Ovi geološki objekti predstavljaju značajne lokalitete za proučavanje trijaskih i jurskih terigeno-karbonatnih sedimenata čiji je naučni značaj iz domena paleontologije, stratigrafije i sedimentologije široko poznat. Cilj ovog rada je reprezentovanje glavnih naučnih argumenata za inventarisanje i zaštitu izdvojenih transgraničnih geoloških objekata koji su jedinstveni po svom sastavu i sadržaju.
PB  - Srpsko geografsko društvo, Beograd
T2  - Glasnik Srpskog geografskog društva
T1  - Review and protection possibilities of some trans-border (East Serbia-West Bulgaria) stratigraphic/palaeontological geosites
T1  - Pregled i mogućnosti zaštite nekih transgraničnih (istočna Srbija-zapadna Bugarska) stratigrafsko-paleontoloških geoobjekata
VL  - 92
IS  - 1
SP  - 171
EP  - 184
UR  - https://hdl.handle.net/21.15107/rcub_gery_500
ER  - 

@article{
author = "Jovanović, Velimir and Carević, Ivana and Vušković, Dragana and Abad, Morteza Taherpour Khalil",
year = "2012",
abstract = "Stratigraphic/palaeontological geosites of Stara Planina Mountain in east Serbia are well developed in the area of Serbian/Bulgarian state border, where with this occassion, three sections of exeptional geological and scientific interest are selected: Jelovica, Rosomač and Senokos. These geosites represent the important localities for study of Triassic and Jurassic terrigene-carbonate deposits, for which the scientific value from the domains of palaeontology, stratigraphy and sedimentology is widely known. The aim of this work is to represent the main scientific arguments for inventory and protection of detached transborder geological sites that are unique according to their composition and content., Stratigrafsko-paleontološki geoobjekti Stare planine istočne Srbije su dobro razvijeni na području srpsko-bugarske državne granice gde su ovom prilikom izdvojena tri profila od izuzetnog geološkog i naučnog značaja: Jelovica, Rosomač i Senokos. Ovi geološki objekti predstavljaju značajne lokalitete za proučavanje trijaskih i jurskih terigeno-karbonatnih sedimenata čiji je naučni značaj iz domena paleontologije, stratigrafije i sedimentologije široko poznat. Cilj ovog rada je reprezentovanje glavnih naučnih argumenata za inventarisanje i zaštitu izdvojenih transgraničnih geoloških objekata koji su jedinstveni po svom sastavu i sadržaju.",
publisher = "Srpsko geografsko društvo, Beograd",
journal = "Glasnik Srpskog geografskog društva",
title = "Review and protection possibilities of some trans-border (East Serbia-West Bulgaria) stratigraphic/palaeontological geosites, Pregled i mogućnosti zaštite nekih transgraničnih (istočna Srbija-zapadna Bugarska) stratigrafsko-paleontoloških geoobjekata",
volume = "92",
number = "1",
pages = "171-184",
url = "https://hdl.handle.net/21.15107/rcub_gery_500"
}

Jovanović, V., Carević, I., Vušković, D.,& Abad, M. T. K.. (2012). Review and protection possibilities of some trans-border (East Serbia-West Bulgaria) stratigraphic/palaeontological geosites. in Glasnik Srpskog geografskog društva
Srpsko geografsko društvo, Beograd., 92(1), 171-184.
https://hdl.handle.net/21.15107/rcub_gery_500

Jovanović V, Carević I, Vušković D, Abad MTK. Review and protection possibilities of some trans-border (East Serbia-West Bulgaria) stratigraphic/palaeontological geosites. in Glasnik Srpskog geografskog društva. 2012;92(1):171-184.
https://hdl.handle.net/21.15107/rcub_gery_500 .

Jovanović, Velimir, Carević, Ivana, Vušković, Dragana, Abad, Morteza Taherpour Khalil, "Review and protection possibilities of some trans-border (East Serbia-West Bulgaria) stratigraphic/palaeontological geosites" in Glasnik Srpskog geografskog društva, 92, no. 1 (2012):171-184,
https://hdl.handle.net/21.15107/rcub_gery_500 .

TY  - JOUR
AU  - Rami, Mahin
AU  - Vaziri, Mohammad Reza
AU  - Abad, Morteza Taherpour Khalil
AU  - Hosseini, Seyed Abolfazl
AU  - Carević, Ivana
AU  - Allameh, Mohsen
PY  - 2012
UR  - https://gery.gef.bg.ac.rs/handle/123456789/488
AB  - The Barremian-Aptian sediments in the Bararig section (Southwest of Kuhbanan) consist of fan alternation of marl and limestone. The palaeontological analysis led to identification of twenty seven taxa of benthic foraminifera and algae in the section studied. Diverse assemblages of benthic foraminifera and also the low planktonic/benthic (P/B) ratio show that the sedimentary environment in the study area was oxygenated and shallow.
PB  - Universidad Nacional Autónoma de México
T2  - Revista Mexicana de Ciencias Geologicas
T1  - Microbiostratigraphy of the Lower Cretaceous strata from the Bararig Mountain, SE Iran
VL  - 29
IS  - 1
SP  - 63
EP  - 75
UR  - https://hdl.handle.net/21.15107/rcub_gery_488
ER  - 

@article{
author = "Rami, Mahin and Vaziri, Mohammad Reza and Abad, Morteza Taherpour Khalil and Hosseini, Seyed Abolfazl and Carević, Ivana and Allameh, Mohsen",
year = "2012",
abstract = "The Barremian-Aptian sediments in the Bararig section (Southwest of Kuhbanan) consist of fan alternation of marl and limestone. The palaeontological analysis led to identification of twenty seven taxa of benthic foraminifera and algae in the section studied. Diverse assemblages of benthic foraminifera and also the low planktonic/benthic (P/B) ratio show that the sedimentary environment in the study area was oxygenated and shallow.",
publisher = "Universidad Nacional Autónoma de México",
journal = "Revista Mexicana de Ciencias Geologicas",
title = "Microbiostratigraphy of the Lower Cretaceous strata from the Bararig Mountain, SE Iran",
volume = "29",
number = "1",
pages = "63-75",
url = "https://hdl.handle.net/21.15107/rcub_gery_488"
}

Rami, M., Vaziri, M. R., Abad, M. T. K., Hosseini, S. A., Carević, I.,& Allameh, M.. (2012). Microbiostratigraphy of the Lower Cretaceous strata from the Bararig Mountain, SE Iran. in Revista Mexicana de Ciencias Geologicas
Universidad Nacional Autónoma de México., 29(1), 63-75.
https://hdl.handle.net/21.15107/rcub_gery_488

Rami M, Vaziri MR, Abad MTK, Hosseini SA, Carević I, Allameh M. Microbiostratigraphy of the Lower Cretaceous strata from the Bararig Mountain, SE Iran. in Revista Mexicana de Ciencias Geologicas. 2012;29(1):63-75.
https://hdl.handle.net/21.15107/rcub_gery_488 .

Rami, Mahin, Vaziri, Mohammad Reza, Abad, Morteza Taherpour Khalil, Hosseini, Seyed Abolfazl, Carević, Ivana, Allameh, Mohsen, "Microbiostratigraphy of the Lower Cretaceous strata from the Bararig Mountain, SE Iran" in Revista Mexicana de Ciencias Geologicas, 29, no. 1 (2012):63-75,
https://hdl.handle.net/21.15107/rcub_gery_488 .

TY  - JOUR
AU  - Ljubović-Obradović, Darivojka
AU  - Carević, Ivana
AU  - Mirković, Monika
AU  - Protić, Nenad
PY  - 2011
UR  - https://gery.gef.bg.ac.rs/handle/123456789/425
AB  - The biostratigraphy of the Upper Cretaceous volcanoclastic-sedimentary formations cropping out in the Timok Eruptive Area of the eastern Serbian Carpatho-Balkanides is presented. Four lithostratigraphic units of formation rank are recognized in the Timok area: Stublica Clastics (Upper Albian/Cenomanian), Ostrelj (Lower Turonian/Santonian), Bor Clastics (Campanian/Maastrichtian) and Bukovo (Campanian/?Maastrichtian). Forty two species of planktonic foraminifera have been determined in the studied area. Eight planktonic foraminiferal zones of Middle Cenomanian through Middle Campanian age have been recognized. These are: Thahnanninella reicheli Interval Zone (Middle Cenomanian), Rotalipora cushmani Taxon Range Zone (Upper Cenomanian), Helvetoglobotruncana helvetica Taxon Range Zone (Lower Turonian), Marginotruncana sigali-Dicarinella primitiva Interval Zone (Upper Turonian to lowermost Coniacian), Dicarinella concavata Interval Zone (Lower Coniacian to lowermost Santonian), Dicarinella asymetrica Taxon Range Zone (Santonian), Globotruncanita elevata Interval Zone (Lower Campanian) and the Globotruncana ventricosa Interval Zone (Middle Campanian). The scarcity or lack of zonal species in the Lower Cenomanian and Upper Campanian/Maastrichtian strata prevents recognition of the nominal zones. The Upper Cretaceous planktonic foraminiferal zones from the Timok Eruptive Area are correlated with coeval zones from adjacent regions of Bulgaria and Romania and from other Tethyan regions.
PB  - Slovak Acad Sciences Geological  Inst, Bratislava
T2  - Geologica Carpathica
T1  - Upper Cretaceous volcanoclastic-sedimentary formations in the Timok Eruptive Area (eastern Serbia): new biostratigraphic data from planktonic foraminifera
VL  - 62
IS  - 5
SP  - 435
EP  - 446
DO  - 10.2478/v10096-011-0031-x
UR  - https://hdl.handle.net/21.15107/rcub_gery_425
ER  - 

@article{
author = "Ljubović-Obradović, Darivojka and Carević, Ivana and Mirković, Monika and Protić, Nenad",
year = "2011",
abstract = "The biostratigraphy of the Upper Cretaceous volcanoclastic-sedimentary formations cropping out in the Timok Eruptive Area of the eastern Serbian Carpatho-Balkanides is presented. Four lithostratigraphic units of formation rank are recognized in the Timok area: Stublica Clastics (Upper Albian/Cenomanian), Ostrelj (Lower Turonian/Santonian), Bor Clastics (Campanian/Maastrichtian) and Bukovo (Campanian/?Maastrichtian). Forty two species of planktonic foraminifera have been determined in the studied area. Eight planktonic foraminiferal zones of Middle Cenomanian through Middle Campanian age have been recognized. These are: Thahnanninella reicheli Interval Zone (Middle Cenomanian), Rotalipora cushmani Taxon Range Zone (Upper Cenomanian), Helvetoglobotruncana helvetica Taxon Range Zone (Lower Turonian), Marginotruncana sigali-Dicarinella primitiva Interval Zone (Upper Turonian to lowermost Coniacian), Dicarinella concavata Interval Zone (Lower Coniacian to lowermost Santonian), Dicarinella asymetrica Taxon Range Zone (Santonian), Globotruncanita elevata Interval Zone (Lower Campanian) and the Globotruncana ventricosa Interval Zone (Middle Campanian). The scarcity or lack of zonal species in the Lower Cenomanian and Upper Campanian/Maastrichtian strata prevents recognition of the nominal zones. The Upper Cretaceous planktonic foraminiferal zones from the Timok Eruptive Area are correlated with coeval zones from adjacent regions of Bulgaria and Romania and from other Tethyan regions.",
publisher = "Slovak Acad Sciences Geological  Inst, Bratislava",
journal = "Geologica Carpathica",
title = "Upper Cretaceous volcanoclastic-sedimentary formations in the Timok Eruptive Area (eastern Serbia): new biostratigraphic data from planktonic foraminifera",
volume = "62",
number = "5",
pages = "435-446",
doi = "10.2478/v10096-011-0031-x",
url = "https://hdl.handle.net/21.15107/rcub_gery_425"
}

Ljubović-Obradović, D., Carević, I., Mirković, M.,& Protić, N.. (2011). Upper Cretaceous volcanoclastic-sedimentary formations in the Timok Eruptive Area (eastern Serbia): new biostratigraphic data from planktonic foraminifera. in Geologica Carpathica
Slovak Acad Sciences Geological  Inst, Bratislava., 62(5), 435-446.
https://doi.org/10.2478/v10096-011-0031-x
https://hdl.handle.net/21.15107/rcub_gery_425

Ljubović-Obradović D, Carević I, Mirković M, Protić N. Upper Cretaceous volcanoclastic-sedimentary formations in the Timok Eruptive Area (eastern Serbia): new biostratigraphic data from planktonic foraminifera. in Geologica Carpathica. 2011;62(5):435-446.
doi:10.2478/v10096-011-0031-x
https://hdl.handle.net/21.15107/rcub_gery_425 .

Ljubović-Obradović, Darivojka, Carević, Ivana, Mirković, Monika, Protić, Nenad, "Upper Cretaceous volcanoclastic-sedimentary formations in the Timok Eruptive Area (eastern Serbia): new biostratigraphic data from planktonic foraminifera" in Geologica Carpathica, 62, no. 5 (2011):435-446,
https://doi.org/10.2478/v10096-011-0031-x .,
https://hdl.handle.net/21.15107/rcub_gery_425 .

TY  - JOUR
AU  - Carević, Ivana
AU  - Radulović, Barbara
AU  - Ljubović-Obradović, Darivojka
AU  - Rabrenović, Dragoman
AU  - Jovanović, Velimir
PY  - 2011
UR  - https://gery.gef.bg.ac.rs/handle/123456789/422
AB  - The Middle Jurassic sediments of the Getic of Carpatho-Balkanides in the trans-border area of Serbia and Romania are insufficiently studied. This zone is composed mainly of pre-Jurassic metamorphic rocks and the Upper Jurassic/Lower Cretaceous limestones. The palaeontological and sedimentological study of the Middle Jurassic deposits of the Brnjica River (Carpatho-Balkanides), which is one of the rare well-exposed outcrops, is being carried out for the first time. The dominant lithologies are grey and yellow sandy limestones and marly limestones with intercalations of reddish shales characterized by low-diversity fossil assemblages dominated by molluscs. Eleven bivalve taxa are determined for the first time in the studied area. Litho-and biofacies analysis in the marine Jurassic strata are reported based on bivalve assemblages with additional data from brachiopods, ammonites and microfossils. The age of the fossil association is determined as the Upper Bajocian and Bathonian based on two brachiopod species Cymathorhynchia quadriplicata and Torquirhynchia asymmetrica. The first is reported from the Middle and the Upper Bajocian sediments and has a wider palaeobiogeographical distribution, while the latter is exclusively described from the Upper Bajocian and Bathonian of the Serbian Carpatho-Balkanides. Most of the collected bivalves have a wider stratigraphic extent. Retroceramus cf. obliquus and Plagiostoma rigidula have up to now been known from the Bajocian stage. The determined macrofauna is compared with the Middle Jurassic fauna of adjacent regions of Hungary, Romania and Bulgaria, and show strong affinity to those of the northern margins of Tethys. By the end of the Bathonian, the depositional environment has changed from shallow-marine to deep-marine, suggesting a drowning of the carbonate platform.
PB  - E Schweizerbartsche Verlagsbuchhandlung, Stuttgart
T2  - Neues Jahrbuch fur Geologie und Palaontologie-Abhandlungen
T1  - First record of a Middle Jurassic macrofauna from the Brnjica (NE Serbia): stratigraphy, palaeoecology and correlation with adjacent regions
VL  - 260
IS  - 3
SP  - 365
EP  - 379
DO  - 10.1127/0077-7749/2011/0148
UR  - https://hdl.handle.net/21.15107/rcub_gery_422
ER  - 

@article{
author = "Carević, Ivana and Radulović, Barbara and Ljubović-Obradović, Darivojka and Rabrenović, Dragoman and Jovanović, Velimir",
year = "2011",
abstract = "The Middle Jurassic sediments of the Getic of Carpatho-Balkanides in the trans-border area of Serbia and Romania are insufficiently studied. This zone is composed mainly of pre-Jurassic metamorphic rocks and the Upper Jurassic/Lower Cretaceous limestones. The palaeontological and sedimentological study of the Middle Jurassic deposits of the Brnjica River (Carpatho-Balkanides), which is one of the rare well-exposed outcrops, is being carried out for the first time. The dominant lithologies are grey and yellow sandy limestones and marly limestones with intercalations of reddish shales characterized by low-diversity fossil assemblages dominated by molluscs. Eleven bivalve taxa are determined for the first time in the studied area. Litho-and biofacies analysis in the marine Jurassic strata are reported based on bivalve assemblages with additional data from brachiopods, ammonites and microfossils. The age of the fossil association is determined as the Upper Bajocian and Bathonian based on two brachiopod species Cymathorhynchia quadriplicata and Torquirhynchia asymmetrica. The first is reported from the Middle and the Upper Bajocian sediments and has a wider palaeobiogeographical distribution, while the latter is exclusively described from the Upper Bajocian and Bathonian of the Serbian Carpatho-Balkanides. Most of the collected bivalves have a wider stratigraphic extent. Retroceramus cf. obliquus and Plagiostoma rigidula have up to now been known from the Bajocian stage. The determined macrofauna is compared with the Middle Jurassic fauna of adjacent regions of Hungary, Romania and Bulgaria, and show strong affinity to those of the northern margins of Tethys. By the end of the Bathonian, the depositional environment has changed from shallow-marine to deep-marine, suggesting a drowning of the carbonate platform.",
publisher = "E Schweizerbartsche Verlagsbuchhandlung, Stuttgart",
journal = "Neues Jahrbuch fur Geologie und Palaontologie-Abhandlungen",
title = "First record of a Middle Jurassic macrofauna from the Brnjica (NE Serbia): stratigraphy, palaeoecology and correlation with adjacent regions",
volume = "260",
number = "3",
pages = "365-379",
doi = "10.1127/0077-7749/2011/0148",
url = "https://hdl.handle.net/21.15107/rcub_gery_422"
}

Carević, I., Radulović, B., Ljubović-Obradović, D., Rabrenović, D.,& Jovanović, V.. (2011). First record of a Middle Jurassic macrofauna from the Brnjica (NE Serbia): stratigraphy, palaeoecology and correlation with adjacent regions. in Neues Jahrbuch fur Geologie und Palaontologie-Abhandlungen
E Schweizerbartsche Verlagsbuchhandlung, Stuttgart., 260(3), 365-379.
https://doi.org/10.1127/0077-7749/2011/0148
https://hdl.handle.net/21.15107/rcub_gery_422

Carević I, Radulović B, Ljubović-Obradović D, Rabrenović D, Jovanović V. First record of a Middle Jurassic macrofauna from the Brnjica (NE Serbia): stratigraphy, palaeoecology and correlation with adjacent regions. in Neues Jahrbuch fur Geologie und Palaontologie-Abhandlungen. 2011;260(3):365-379.
doi:10.1127/0077-7749/2011/0148
https://hdl.handle.net/21.15107/rcub_gery_422 .

Carević, Ivana, Radulović, Barbara, Ljubović-Obradović, Darivojka, Rabrenović, Dragoman, Jovanović, Velimir, "First record of a Middle Jurassic macrofauna from the Brnjica (NE Serbia): stratigraphy, palaeoecology and correlation with adjacent regions" in Neues Jahrbuch fur Geologie und Palaontologie-Abhandlungen, 260, no. 3 (2011):365-379,
https://doi.org/10.1127/0077-7749/2011/0148 .,
https://hdl.handle.net/21.15107/rcub_gery_422 .

TY  - JOUR
AU  - Carević, Ivana
AU  - Ljubović-Obradović, Darivojka
AU  - Božinović, Monika
AU  - Jovanović, Velimir
PY  - 2010
UR  - https://gery.gef.bg.ac.rs/handle/123456789/337
AB  - The Upper Barremian-Lower Aptian succession is recorded from a limestone sequence that crops out in the surrounding of Rakova Bara in the Carpatho-Balkanides range in northeastern Serbia. The micropalaeontological and sedimentological studies lead to recognition of the two types of microfacies. The benthic foraminiferal association consists of Vercorsella laurentii, Rumanoloculina robusta, Praechrysalidina infracretaceae, Dictyoconus gr. arabicus, Debarina hahounerensis, Charentia cuvilieri and Pseudocyclammina lituus that confirm the stratigraphical and palaeoenvironmental connection of the microfossil assemblages with the classical Urgonian-type, shallow-water carbonate sedimentation. The association documented for the first time in the study area is considered typical of the Tethyan Realm. The stratigraphical position of the benthic foraminifera species within the Upper Barremian-Lower Aptian interval is discussed. The Urgonian Limestone's of the studied section are comparable with adjacent areas of eastern Serbia and Romanian South Carpathians.
AB  - U radu je prikazana gornjobaremsko-donjoaptska sukcesija sedimenata otkrivenih u okolini sela Rakova bara u severoistočnoj Srbiji. Mikropaleontološkim i sedimentološkim istraživanjima su izdvojena dva tipa mikrofacija. U okviru bentoske foraminiferske asocijacije su utvrđene sledeće vrste: Vercorsella laurentii, Rumanoloculina robusta, Praechrysalidina infracretaceae, Dictyoconus gr. arabicus, Debarina hahounerensis, Charentia cuvilieri i Pseudocyclammina lituus čije stratigrafsko rasprostranjenje u okviru definisanih depozicionih sredina ukazuje na klasično urgonsko razviće ovih sedimenata. Determinisana mikroasocijacija je tipična za Tetis i dokumentovana je po prvi put u ovom delu Karpato-balkanida severoistočne Srbije. Stratigrafska pozicija determinisanih vrsta je diskutovana i izvršeno je poređenje ovih tvorevina sa susednim oblastima istočne Srbije i Južnih Karpata Rumunije sa kojima pokazuju veliku sličnost.
PB  - Srpsko geografsko društvo, Beograd
T2  - Glasnik Srpskog geografskog društva
T1  - Upper Barremian-Lower Aptian Urgonian limestone's in the Rakova bara section (Carpatho-balkanides, NE Serbia): Analysis and comparison with adjacent areas
T1  - Urgonski krečnjaci gornjeg barema i donjeg apta Rakove bare (Karpato-balkanidi, SI Srbija) - analiza i poređenje sa susednim oblastima
VL  - 90
IS  - 1
SP  - 1
EP  - 16
UR  - https://hdl.handle.net/21.15107/rcub_gery_337
ER  - 

@article{
author = "Carević, Ivana and Ljubović-Obradović, Darivojka and Božinović, Monika and Jovanović, Velimir",
year = "2010",
abstract = "The Upper Barremian-Lower Aptian succession is recorded from a limestone sequence that crops out in the surrounding of Rakova Bara in the Carpatho-Balkanides range in northeastern Serbia. The micropalaeontological and sedimentological studies lead to recognition of the two types of microfacies. The benthic foraminiferal association consists of Vercorsella laurentii, Rumanoloculina robusta, Praechrysalidina infracretaceae, Dictyoconus gr. arabicus, Debarina hahounerensis, Charentia cuvilieri and Pseudocyclammina lituus that confirm the stratigraphical and palaeoenvironmental connection of the microfossil assemblages with the classical Urgonian-type, shallow-water carbonate sedimentation. The association documented for the first time in the study area is considered typical of the Tethyan Realm. The stratigraphical position of the benthic foraminifera species within the Upper Barremian-Lower Aptian interval is discussed. The Urgonian Limestone's of the studied section are comparable with adjacent areas of eastern Serbia and Romanian South Carpathians., U radu je prikazana gornjobaremsko-donjoaptska sukcesija sedimenata otkrivenih u okolini sela Rakova bara u severoistočnoj Srbiji. Mikropaleontološkim i sedimentološkim istraživanjima su izdvojena dva tipa mikrofacija. U okviru bentoske foraminiferske asocijacije su utvrđene sledeće vrste: Vercorsella laurentii, Rumanoloculina robusta, Praechrysalidina infracretaceae, Dictyoconus gr. arabicus, Debarina hahounerensis, Charentia cuvilieri i Pseudocyclammina lituus čije stratigrafsko rasprostranjenje u okviru definisanih depozicionih sredina ukazuje na klasično urgonsko razviće ovih sedimenata. Determinisana mikroasocijacija je tipična za Tetis i dokumentovana je po prvi put u ovom delu Karpato-balkanida severoistočne Srbije. Stratigrafska pozicija determinisanih vrsta je diskutovana i izvršeno je poređenje ovih tvorevina sa susednim oblastima istočne Srbije i Južnih Karpata Rumunije sa kojima pokazuju veliku sličnost.",
publisher = "Srpsko geografsko društvo, Beograd",
journal = "Glasnik Srpskog geografskog društva",
title = "Upper Barremian-Lower Aptian Urgonian limestone's in the Rakova bara section (Carpatho-balkanides, NE Serbia): Analysis and comparison with adjacent areas, Urgonski krečnjaci gornjeg barema i donjeg apta Rakove bare (Karpato-balkanidi, SI Srbija) - analiza i poređenje sa susednim oblastima",
volume = "90",
number = "1",
pages = "1-16",
url = "https://hdl.handle.net/21.15107/rcub_gery_337"
}

Carević, I., Ljubović-Obradović, D., Božinović, M.,& Jovanović, V.. (2010). Upper Barremian-Lower Aptian Urgonian limestone's in the Rakova bara section (Carpatho-balkanides, NE Serbia): Analysis and comparison with adjacent areas. in Glasnik Srpskog geografskog društva
Srpsko geografsko društvo, Beograd., 90(1), 1-16.
https://hdl.handle.net/21.15107/rcub_gery_337

Carević I, Ljubović-Obradović D, Božinović M, Jovanović V. Upper Barremian-Lower Aptian Urgonian limestone's in the Rakova bara section (Carpatho-balkanides, NE Serbia): Analysis and comparison with adjacent areas. in Glasnik Srpskog geografskog društva. 2010;90(1):1-16.
https://hdl.handle.net/21.15107/rcub_gery_337 .

Carević, Ivana, Ljubović-Obradović, Darivojka, Božinović, Monika, Jovanović, Velimir, "Upper Barremian-Lower Aptian Urgonian limestone's in the Rakova bara section (Carpatho-balkanides, NE Serbia): Analysis and comparison with adjacent areas" in Glasnik Srpskog geografskog društva, 90, no. 1 (2010):1-16,
https://hdl.handle.net/21.15107/rcub_gery_337 .

TY  - JOUR
AU  - Carević, Ivana
AU  - Milinčić, Miroljub
AU  - Jovanović, Velimir
PY  - 2009
UR  - https://gery.gef.bg.ac.rs/handle/123456789/300
AB  - Aleksandrovac Zupa represents the example of territorial area with composite geological structure and furthermore compound geotectonic framework. Due to the character of some formations, framework and time relation of deformation, these areas belong among the most compound on the Balkan Peninsula. On its territory, the big and composite structural-facies zones are being confronted and became imbued. In a stratigraphic point of view, the largest extend have the Miocene deposits that overlain the crystalline schists of Proterozoic. .
AB  - Aleksandrovačka Župa predstavlja primer teritorijalne celine složenog geološkog sastava i još složenijeg geotektonskog sklopa. Prema karakteru pojedinih formacija, sklopu i vremenskim odnosi-ma deformacija ovi tereni spadaju među najsloženije na Balkanskom poluostrvu. Na njenoj teritoriji se sučeljavaju i prožimaju velike i složene strukturno-facijalne zone. U stratigrafskom pogledu najveće rasprostranjenje imaju miocenske tvorevine koje predstavljaju povlatu kristalastim škriljcima proterozoika. .
PB  - Srpsko geografsko društvo, Beograd
T2  - Glasnik Srpskog geografskog društva
T1  - Contribution to the study of geological setting of lower Aleksandrovac Zupa
T1  - Prilog poznavanju geologije donje Aleksandrovačke Župe
VL  - 89
IS  - 3
SP  - 135
EP  - 146
UR  - https://hdl.handle.net/21.15107/rcub_gery_300
ER  - 

@article{
author = "Carević, Ivana and Milinčić, Miroljub and Jovanović, Velimir",
year = "2009",
abstract = "Aleksandrovac Zupa represents the example of territorial area with composite geological structure and furthermore compound geotectonic framework. Due to the character of some formations, framework and time relation of deformation, these areas belong among the most compound on the Balkan Peninsula. On its territory, the big and composite structural-facies zones are being confronted and became imbued. In a stratigraphic point of view, the largest extend have the Miocene deposits that overlain the crystalline schists of Proterozoic. ., Aleksandrovačka Župa predstavlja primer teritorijalne celine složenog geološkog sastava i još složenijeg geotektonskog sklopa. Prema karakteru pojedinih formacija, sklopu i vremenskim odnosi-ma deformacija ovi tereni spadaju među najsloženije na Balkanskom poluostrvu. Na njenoj teritoriji se sučeljavaju i prožimaju velike i složene strukturno-facijalne zone. U stratigrafskom pogledu najveće rasprostranjenje imaju miocenske tvorevine koje predstavljaju povlatu kristalastim škriljcima proterozoika. .",
publisher = "Srpsko geografsko društvo, Beograd",
journal = "Glasnik Srpskog geografskog društva",
title = "Contribution to the study of geological setting of lower Aleksandrovac Zupa, Prilog poznavanju geologije donje Aleksandrovačke Župe",
volume = "89",
number = "3",
pages = "135-146",
url = "https://hdl.handle.net/21.15107/rcub_gery_300"
}

Carević, I., Milinčić, M.,& Jovanović, V.. (2009). Contribution to the study of geological setting of lower Aleksandrovac Zupa. in Glasnik Srpskog geografskog društva
Srpsko geografsko društvo, Beograd., 89(3), 135-146.
https://hdl.handle.net/21.15107/rcub_gery_300

Carević I, Milinčić M, Jovanović V. Contribution to the study of geological setting of lower Aleksandrovac Zupa. in Glasnik Srpskog geografskog društva. 2009;89(3):135-146.
https://hdl.handle.net/21.15107/rcub_gery_300 .

Carević, Ivana, Milinčić, Miroljub, Jovanović, Velimir, "Contribution to the study of geological setting of lower Aleksandrovac Zupa" in Glasnik Srpskog geografskog društva, 89, no. 3 (2009):135-146,
https://hdl.handle.net/21.15107/rcub_gery_300 .

TY  - JOUR
AU  - Carević, Ivana
AU  - Jovanović, Velimir
PY  - 2009
UR  - https://gery.gef.bg.ac.rs/handle/123456789/294
AB  - The analysis of stratigraphic-structural features of Mačva basin had been conducted in this paper on the basis of data obtained with deep exploratory boring performed for the needs of hydrogeothermal research project for the purpose of identifying the reserves of geothermal energy of Mačva. The research has been carried out with the aim of finding out the relation between the Tertiary and its Triassic bedrock (Ladinian and Carnian stages) in which process the considerable realistic image of paleorelief (the bedrock of Tertiary deposits) was obtained.
AB  - U radu je izvršena analiza stratigrafsko-tektonskih karakteristika basena Mačve na osnovu podataka koji su dobijeni dubokim istražnim bušenjem rađenim za potrebe projekta hidrogeotermalnih istraživanja u cilju utvrđivanja rezervi geotermalne energije Mačve. Sprovedeno je istraživanje čiji je cilj bio utvrđivanje odnosa između tercijara i njegove trijaske podloge (ladinski i karnijski kat) pri čemu je dobijena dosta realna slika o izgledu paleoreljefa (podloga tercijarnih sedimenata).
PB  - Srpsko geografsko društvo, Beograd
T2  - Glasnik Srpskog geografskog društva
T1  - Stratigraphic-structural characteristics of Mačva basin
T1  - Stratigrafsko-tektonske karakteristike mačvanskog basena
VL  - 89
IS  - 4
SP  - 121
EP  - 139
UR  - https://hdl.handle.net/21.15107/rcub_gery_294
ER  - 

@article{
author = "Carević, Ivana and Jovanović, Velimir",
year = "2009",
abstract = "The analysis of stratigraphic-structural features of Mačva basin had been conducted in this paper on the basis of data obtained with deep exploratory boring performed for the needs of hydrogeothermal research project for the purpose of identifying the reserves of geothermal energy of Mačva. The research has been carried out with the aim of finding out the relation between the Tertiary and its Triassic bedrock (Ladinian and Carnian stages) in which process the considerable realistic image of paleorelief (the bedrock of Tertiary deposits) was obtained., U radu je izvršena analiza stratigrafsko-tektonskih karakteristika basena Mačve na osnovu podataka koji su dobijeni dubokim istražnim bušenjem rađenim za potrebe projekta hidrogeotermalnih istraživanja u cilju utvrđivanja rezervi geotermalne energije Mačve. Sprovedeno je istraživanje čiji je cilj bio utvrđivanje odnosa između tercijara i njegove trijaske podloge (ladinski i karnijski kat) pri čemu je dobijena dosta realna slika o izgledu paleoreljefa (podloga tercijarnih sedimenata).",
publisher = "Srpsko geografsko društvo, Beograd",
journal = "Glasnik Srpskog geografskog društva",
title = "Stratigraphic-structural characteristics of Mačva basin, Stratigrafsko-tektonske karakteristike mačvanskog basena",
volume = "89",
number = "4",
pages = "121-139",
url = "https://hdl.handle.net/21.15107/rcub_gery_294"
}

Carević, I.,& Jovanović, V.. (2009). Stratigraphic-structural characteristics of Mačva basin. in Glasnik Srpskog geografskog društva
Srpsko geografsko društvo, Beograd., 89(4), 121-139.
https://hdl.handle.net/21.15107/rcub_gery_294

Carević I, Jovanović V. Stratigraphic-structural characteristics of Mačva basin. in Glasnik Srpskog geografskog društva. 2009;89(4):121-139.
https://hdl.handle.net/21.15107/rcub_gery_294 .

Carević, Ivana, Jovanović, Velimir, "Stratigraphic-structural characteristics of Mačva basin" in Glasnik Srpskog geografskog društva, 89, no. 4 (2009):121-139,
https://hdl.handle.net/21.15107/rcub_gery_294 .

TY  - JOUR
AU  - Carević, Ivana
AU  - Jovanović, Velimir
PY  - 2007
UR  - https://gery.gef.bg.ac.rs/handle/123456789/205
AB  - Kučaj basin and Suva planina basin belong to the northern part of Carpathian Balkan belt and cover the area of Golubac mountains. This part of Carpathian Balkanides during the Jurrasic and Cretaceus period represented marine environment with dominate carbonate sedimentation. In this paper on the basis of the study of the fossil remains an attempt was made of their environment reconstruction, their way and conditions of life.
AB  - Kučajski i suvoplaninski basen pripadaju severnom delu Karpato-balkanskog pojasa i obuhvataju oblast Golubačkih planina. Ovaj deo Karpato-balkanida je tokom jure i krede predstavljao marinsku sredinu sa dominantnom karbonatnom sedimentacijom. U okviru ovog rada na osnovu proučavanja fosilnih ostataka organizama izvršen je pokušaj rekonstrukcije sredine u kojoj su ti organizmi egzistovali, njihov način i uslovi života.
PB  - Univerzitet u Beogradu - Geografski fakultet, Beograd
T2  - Zbornik radova - Geografski fakultet Univerziteta u Beogradu
T1  - Paleoecologic showing of depositing environment of Jurassic and cretaceous sediments in the area of Golubac mountains
T1  - Paleoekološki prikaz sredine taloženja jurskih i krednih sedimenata na području Golubačkih planina
IS  - 55
SP  - 23
EP  - 28
UR  - https://hdl.handle.net/21.15107/rcub_gery_205
ER  - 

@article{
author = "Carević, Ivana and Jovanović, Velimir",
year = "2007",
abstract = "Kučaj basin and Suva planina basin belong to the northern part of Carpathian Balkan belt and cover the area of Golubac mountains. This part of Carpathian Balkanides during the Jurrasic and Cretaceus period represented marine environment with dominate carbonate sedimentation. In this paper on the basis of the study of the fossil remains an attempt was made of their environment reconstruction, their way and conditions of life., Kučajski i suvoplaninski basen pripadaju severnom delu Karpato-balkanskog pojasa i obuhvataju oblast Golubačkih planina. Ovaj deo Karpato-balkanida je tokom jure i krede predstavljao marinsku sredinu sa dominantnom karbonatnom sedimentacijom. U okviru ovog rada na osnovu proučavanja fosilnih ostataka organizama izvršen je pokušaj rekonstrukcije sredine u kojoj su ti organizmi egzistovali, njihov način i uslovi života.",
publisher = "Univerzitet u Beogradu - Geografski fakultet, Beograd",
journal = "Zbornik radova - Geografski fakultet Univerziteta u Beogradu",
title = "Paleoecologic showing of depositing environment of Jurassic and cretaceous sediments in the area of Golubac mountains, Paleoekološki prikaz sredine taloženja jurskih i krednih sedimenata na području Golubačkih planina",
number = "55",
pages = "23-28",
url = "https://hdl.handle.net/21.15107/rcub_gery_205"
}

Carević, I.,& Jovanović, V.. (2007). Paleoecologic showing of depositing environment of Jurassic and cretaceous sediments in the area of Golubac mountains. in Zbornik radova - Geografski fakultet Univerziteta u Beogradu
Univerzitet u Beogradu - Geografski fakultet, Beograd.(55), 23-28.
https://hdl.handle.net/21.15107/rcub_gery_205

Carević I, Jovanović V. Paleoecologic showing of depositing environment of Jurassic and cretaceous sediments in the area of Golubac mountains. in Zbornik radova - Geografski fakultet Univerziteta u Beogradu. 2007;(55):23-28.
https://hdl.handle.net/21.15107/rcub_gery_205 .

Carević, Ivana, Jovanović, Velimir, "Paleoecologic showing of depositing environment of Jurassic and cretaceous sediments in the area of Golubac mountains" in Zbornik radova - Geografski fakultet Univerziteta u Beogradu, no. 55 (2007):23-28,
https://hdl.handle.net/21.15107/rcub_gery_205 .