TY  - JOUR
AU  - Taherpour-Khalil-Abad, Morteza
AU  - Carević, Ivana
AU  - Bahremand, Maryam
AU  - Mojtahedin, Elham
PY  - 2019
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1676
AB  - This paper is to present the biostratigraphy of the Maastrichtian Kalat Formation in Karnaveh area of the northeastern Iranian Kopet-Dagh sedimentary basin. Micropaleontological studies have led to the determination of micro-calcite structures, having Microcodium deposited in the stratigraphic section due to transgression and regression of the sea. On the basis of determined benthic foraminiferal taxa Laffitteina mengaudi (Astre), Lepidorbitoides socialis (Leymerie), Omphalocyclus macroporus (Lamarck), Orbitoides apiculata Schlumberger, Orbitoides media (d’Archiac), Rotalia
skourensis Pfender, Siderolites calcitrapoides Lamarck, Sirtina orbitoidiformis Brönnimann & Wirz, Sulcoperculina cosdeni Applin & Jordan, Sulcoperculina globosa Cizancourt and Sulcoperculina vermunti (Thiadens), Kalat Formation in the studied stratigraphic section is assigned to the Maastrichtian. The current study represents the first record of Microcodium occurrence in Kopet-Dagh sedimentary basin in northeast Iran, expanding the current knowledge on its palaeogeographical distribution in Tethyan Realm.
PB  - Geoscience Museum of Mashhad
T2  - Iranian Journal of Geoscience Museum
T1  - The First Record of Microcodium from Maastrichtian Kalat Formation, Kopet-Dagh Sedimentary Basin, NE Iran: Biostratigraphy and Microfacies
VL  - 1
IS  - 1
SP  - 5
EP  - 11
UR  - https://hdl.handle.net/21.15107/rcub_gery_1676
ER  - 

@article{
author = "Taherpour-Khalil-Abad, Morteza and Carević, Ivana and Bahremand, Maryam and Mojtahedin, Elham",
year = "2019",
abstract = "This paper is to present the biostratigraphy of the Maastrichtian Kalat Formation in Karnaveh area of the northeastern Iranian Kopet-Dagh sedimentary basin. Micropaleontological studies have led to the determination of micro-calcite structures, having Microcodium deposited in the stratigraphic section due to transgression and regression of the sea. On the basis of determined benthic foraminiferal taxa Laffitteina mengaudi (Astre), Lepidorbitoides socialis (Leymerie), Omphalocyclus macroporus (Lamarck), Orbitoides apiculata Schlumberger, Orbitoides media (d’Archiac), Rotalia
skourensis Pfender, Siderolites calcitrapoides Lamarck, Sirtina orbitoidiformis Brönnimann & Wirz, Sulcoperculina cosdeni Applin & Jordan, Sulcoperculina globosa Cizancourt and Sulcoperculina vermunti (Thiadens), Kalat Formation in the studied stratigraphic section is assigned to the Maastrichtian. The current study represents the first record of Microcodium occurrence in Kopet-Dagh sedimentary basin in northeast Iran, expanding the current knowledge on its palaeogeographical distribution in Tethyan Realm.",
publisher = "Geoscience Museum of Mashhad",
journal = "Iranian Journal of Geoscience Museum",
title = "The First Record of Microcodium from Maastrichtian Kalat Formation, Kopet-Dagh Sedimentary Basin, NE Iran: Biostratigraphy and Microfacies",
volume = "1",
number = "1",
pages = "5-11",
url = "https://hdl.handle.net/21.15107/rcub_gery_1676"
}

Taherpour-Khalil-Abad, M., Carević, I., Bahremand, M.,& Mojtahedin, E.. (2019). The First Record of Microcodium from Maastrichtian Kalat Formation, Kopet-Dagh Sedimentary Basin, NE Iran: Biostratigraphy and Microfacies. in Iranian Journal of Geoscience Museum
Geoscience Museum of Mashhad., 1(1), 5-11.
https://hdl.handle.net/21.15107/rcub_gery_1676

Taherpour-Khalil-Abad M, Carević I, Bahremand M, Mojtahedin E. The First Record of Microcodium from Maastrichtian Kalat Formation, Kopet-Dagh Sedimentary Basin, NE Iran: Biostratigraphy and Microfacies. in Iranian Journal of Geoscience Museum. 2019;1(1):5-11.
https://hdl.handle.net/21.15107/rcub_gery_1676 .

Taherpour-Khalil-Abad, Morteza, Carević, Ivana, Bahremand, Maryam, Mojtahedin, Elham, "The First Record of Microcodium from Maastrichtian Kalat Formation, Kopet-Dagh Sedimentary Basin, NE Iran: Biostratigraphy and Microfacies" in Iranian Journal of Geoscience Museum, 1, no. 1 (2019):5-11,
https://hdl.handle.net/21.15107/rcub_gery_1676 .

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  - Beograd : Univerzitet u Beogradu - Rudarsko-geološki fakultet
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 = "Beograd : Univerzitet u Beogradu - Rudarsko-geološki fakultet",
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
Beograd : Univerzitet u Beogradu - Rudarsko-geološki fakultet., 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  - 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  - 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  - 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  - 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  - 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  - Beograd : Srpsko geografsko društvo
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 = "Beograd : Srpsko geografsko društvo",
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
Beograd : Srpsko geografsko društvo., 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 .