GERY - Faculty of Geography Repository
University of Belgrade - Faculty of Geography
    • English
    • Serbian (Cyrillic)
    • Serbian (Latin)
  • English 
    • English
    • Serbian (Cyrillic)
    • Serbian (Latin)
  • Login
View Item 
  •   GERY
  • Geografski fakultet
  • Radovi istraživača
  • View Item
  •   GERY
  • Geografski fakultet
  • Radovi istraživača
  • View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.

Comparisons between the Urgonian platform carbonates from eastern Serbia (Carpatho-Balkanides) and northeast Iran (Kopet-Dagh Basin): Depositional facies, microfacies, biostratigraphy, palaeoenvironments and palaeoecology

Authorized Users Only
2013
Authors
Carević, Ivana
Abad, Morteza Taherpour Khalil
Ljubović-Obradović, Darivojka
Vaziri, Seyed Hamid
Mirković, Monika
Aryaei, Ali Asghar
Stejić, Petar
Ashouri, Ali Reza
Article (Published version)
Metadata
Show full item record
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 a...nd 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.

Keywords:
Barremian/Early Aptian / Getic / Tirgan Formation / Benthic foraminifera / Calcareous algae
Source:
Cretaceous Research, 2013, 40, 110-130
Publisher:
  • Academic Press Ltd- Elsevier Science Ltd, London
Funding / projects:
  • Ministry of Science and Technological Development of the Republic of Serbia

DOI: 10.1016/j.cretres.2012.06.003

ISSN: 0195-6671

WoS: 000312685200011

Scopus: 2-s2.0-84870321148
[ Google Scholar ]
20
17
Handle
https://hdl.handle.net/21.15107/rcub_gery_598
URI
https://gery.gef.bg.ac.rs/handle/123456789/598
Collections
  • Radovi istraživača
Institution/Community
Geografski fakultet
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 .

DSpace software copyright © 2002-2015  DuraSpace
About GERY - GEography RepositoRY | Send Feedback

OpenAIRERCUB
 

 

All of DSpaceCommunitiesAuthorsTitlesSubjectsThis institutionAuthorsTitlesSubjects

Statistics

View Usage Statistics

DSpace software copyright © 2002-2015  DuraSpace
About GERY - GEography RepositoRY | Send Feedback

OpenAIRERCUB