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 .