THE RESERVOIR POTENTIAL OF MIOCENE CARBONATE ROCKS IN THE ASKALE AND HINIS‐MUS‐VAN SUB‐BASINS, EAST ANATOLIA, TURKEY
Lower‐middle Miocene limestones in East Anatolia (eastern Turkey) assigned to the Adilcevaz Formation were studied using core and cuttings data from eight wells in the Tertiary Askale and Hinis‐Mus‐Van sub‐basins. Their depositional environment, diagenetic characteristics and reservoir quality are r...
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crwiley:10.1111/j.1747-5457.2003.tb00024.x 2024-04-28T08:36:30+00:00 THE RESERVOIR POTENTIAL OF MIOCENE CARBONATE ROCKS IN THE ASKALE AND HINIS‐MUS‐VAN SUB‐BASINS, EAST ANATOLIA, TURKEY Büyükutku, A. G. 2003 http://dx.doi.org/10.1111/j.1747-5457.2003.tb00024.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1747-5457.2003.tb00024.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1747-5457.2003.tb00024.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Petroleum Geology volume 26, issue 2, page 175-188 ISSN 0141-6421 1747-5457 Earth and Planetary Sciences (miscellaneous) Geology Energy Engineering and Power Technology Fuel Technology journal-article 2003 crwiley https://doi.org/10.1111/j.1747-5457.2003.tb00024.x 2024-04-02T08:46:19Z Lower‐middle Miocene limestones in East Anatolia (eastern Turkey) assigned to the Adilcevaz Formation were studied using core and cuttings data from eight wells in the Tertiary Askale and Hinis‐Mus‐Van sub‐basins. Their depositional environment, diagenetic characteristics and reservoir quality are reviewed. The Adilcevaz Formation carbonates are up to 225m thick. Abundant bioclasts are dominated by corals, encrusting red algae, bryozoans, and benthonic and planktonic foraminifera. Reef‐core, fore‐reef and back‐reef facies were recognized. The preservation of primary porosity is generally poor as a result of late calcite cementation. Porosity is mainly present as moulds, vugs and interparticle types, which are best developed in the fore‐reef and reef‐core facies. However these pores are poorly connected and permeability is generally less than 0.1 mD. In contrast to coeval limestones of similiar facies in Iran, Iraq and other parts of the Middle East, the Adilcevaz Formation has little reservoir potential. Article in Journal/Newspaper Planktonic foraminifera Wiley Online Library Journal of Petroleum Geology 26 2 175 188 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
topic |
Earth and Planetary Sciences (miscellaneous) Geology Energy Engineering and Power Technology Fuel Technology |
spellingShingle |
Earth and Planetary Sciences (miscellaneous) Geology Energy Engineering and Power Technology Fuel Technology Büyükutku, A. G. THE RESERVOIR POTENTIAL OF MIOCENE CARBONATE ROCKS IN THE ASKALE AND HINIS‐MUS‐VAN SUB‐BASINS, EAST ANATOLIA, TURKEY |
topic_facet |
Earth and Planetary Sciences (miscellaneous) Geology Energy Engineering and Power Technology Fuel Technology |
description |
Lower‐middle Miocene limestones in East Anatolia (eastern Turkey) assigned to the Adilcevaz Formation were studied using core and cuttings data from eight wells in the Tertiary Askale and Hinis‐Mus‐Van sub‐basins. Their depositional environment, diagenetic characteristics and reservoir quality are reviewed. The Adilcevaz Formation carbonates are up to 225m thick. Abundant bioclasts are dominated by corals, encrusting red algae, bryozoans, and benthonic and planktonic foraminifera. Reef‐core, fore‐reef and back‐reef facies were recognized. The preservation of primary porosity is generally poor as a result of late calcite cementation. Porosity is mainly present as moulds, vugs and interparticle types, which are best developed in the fore‐reef and reef‐core facies. However these pores are poorly connected and permeability is generally less than 0.1 mD. In contrast to coeval limestones of similiar facies in Iran, Iraq and other parts of the Middle East, the Adilcevaz Formation has little reservoir potential. |
format |
Article in Journal/Newspaper |
author |
Büyükutku, A. G. |
author_facet |
Büyükutku, A. G. |
author_sort |
Büyükutku, A. G. |
title |
THE RESERVOIR POTENTIAL OF MIOCENE CARBONATE ROCKS IN THE ASKALE AND HINIS‐MUS‐VAN SUB‐BASINS, EAST ANATOLIA, TURKEY |
title_short |
THE RESERVOIR POTENTIAL OF MIOCENE CARBONATE ROCKS IN THE ASKALE AND HINIS‐MUS‐VAN SUB‐BASINS, EAST ANATOLIA, TURKEY |
title_full |
THE RESERVOIR POTENTIAL OF MIOCENE CARBONATE ROCKS IN THE ASKALE AND HINIS‐MUS‐VAN SUB‐BASINS, EAST ANATOLIA, TURKEY |
title_fullStr |
THE RESERVOIR POTENTIAL OF MIOCENE CARBONATE ROCKS IN THE ASKALE AND HINIS‐MUS‐VAN SUB‐BASINS, EAST ANATOLIA, TURKEY |
title_full_unstemmed |
THE RESERVOIR POTENTIAL OF MIOCENE CARBONATE ROCKS IN THE ASKALE AND HINIS‐MUS‐VAN SUB‐BASINS, EAST ANATOLIA, TURKEY |
title_sort |
reservoir potential of miocene carbonate rocks in the askale and hinis‐mus‐van sub‐basins, east anatolia, turkey |
publisher |
Wiley |
publishDate |
2003 |
url |
http://dx.doi.org/10.1111/j.1747-5457.2003.tb00024.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1747-5457.2003.tb00024.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1747-5457.2003.tb00024.x |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
Journal of Petroleum Geology volume 26, issue 2, page 175-188 ISSN 0141-6421 1747-5457 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1747-5457.2003.tb00024.x |
container_title |
Journal of Petroleum Geology |
container_volume |
26 |
container_issue |
2 |
container_start_page |
175 |
op_container_end_page |
188 |
_version_ |
1797568257364852736 |