Hydrocarbon Generation Potential of Chia Gara Formation in Three Selected Wells, Northern Iraq
In this study collected samples of Chia Gara Formation in Atrush, Shaikhan and Sarsang oilfields are used to geochemical characteristics of organic matter in this formation. This determination was based on Rock-Eval pyrolysis and Biomarker analyses. The Chia Gara Formation can be considered as good...
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Online Access: | https://doi.org/10.1515/geo-2019-0007 |
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doaj-b685dc723b8f49229f5379f55a9f5a322021-09-05T20:50:49ZengDe GruyterOpen Geosciences2391-54472019-03-01111778810.1515/geo-2019-0007geo-2019-0007Hydrocarbon Generation Potential of Chia Gara Formation in Three Selected Wells, Northern IraqMamaseni Wrya J.0Naqshabandi Srood F1Al-Jaboury Falah Kh.2Department of Geology, College of Science, Salahaddin University, Erbil, IraqDepartment of Geology, College of Science, Salahaddin University, Erbil, IraqPetroleum Engineering Department, Knowledge Private University, Erbil, IraqIn this study collected samples of Chia Gara Formation in Atrush, Shaikhan and Sarsang oilfields are used to geochemical characteristics of organic matter in this formation. This determination was based on Rock-Eval pyrolysis and Biomarker analyses. The Chia Gara Formation can be considered as good to excellent source rock; it’s TOC content ranges from 1.14-8.5wt% with an average of 1.85%, 3.91%, and 6.94% in Atush-1, Mangesh-1 and Shaikhan-8 wells respectively. The samples of Chia Gara Formation contain kerogen type II. These properties are considered optimal for oil generation. The low oxygen index (OI) and pristane/phytane (Pr/Ph) ratios (Average 20.73, 0.61 respectively) and high hydrogen index (HI) (average 637.6) indicate that the formation was deposited under anoxic condition. According to regular sterane (C27%, C28%, C29%) and terpanes ratios (C29/C30, C31/C30 hopane), the formation was deposited in marine environment.https://doi.org/10.1515/geo-2019-0007chia gara formation, anoxic condition, biomarker assemblagetype ii kerogenmature organic matteroil-prone |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Mamaseni Wrya J. Naqshabandi Srood F Al-Jaboury Falah Kh. |
spellingShingle |
Mamaseni Wrya J. Naqshabandi Srood F Al-Jaboury Falah Kh. Hydrocarbon Generation Potential of Chia Gara Formation in Three Selected Wells, Northern Iraq Open Geosciences chia gara formation, anoxic condition, biomarker assemblage type ii kerogen mature organic matter oil-prone |
author_facet |
Mamaseni Wrya J. Naqshabandi Srood F Al-Jaboury Falah Kh. |
author_sort |
Mamaseni Wrya J. |
title |
Hydrocarbon Generation Potential of Chia Gara Formation in Three Selected Wells, Northern Iraq |
title_short |
Hydrocarbon Generation Potential of Chia Gara Formation in Three Selected Wells, Northern Iraq |
title_full |
Hydrocarbon Generation Potential of Chia Gara Formation in Three Selected Wells, Northern Iraq |
title_fullStr |
Hydrocarbon Generation Potential of Chia Gara Formation in Three Selected Wells, Northern Iraq |
title_full_unstemmed |
Hydrocarbon Generation Potential of Chia Gara Formation in Three Selected Wells, Northern Iraq |
title_sort |
hydrocarbon generation potential of chia gara formation in three selected wells, northern iraq |
publisher |
De Gruyter |
series |
Open Geosciences |
issn |
2391-5447 |
publishDate |
2019-03-01 |
description |
In this study collected samples of Chia Gara Formation in Atrush, Shaikhan and Sarsang oilfields are used to geochemical characteristics of organic matter in this formation. This determination was based on Rock-Eval pyrolysis and Biomarker analyses. The Chia Gara Formation can be considered as good to excellent source rock; it’s TOC content ranges from 1.14-8.5wt% with an average of 1.85%, 3.91%, and 6.94% in Atush-1, Mangesh-1 and Shaikhan-8 wells respectively. The samples of Chia Gara Formation contain kerogen type II. These properties are considered optimal for oil generation. The low oxygen index (OI) and pristane/phytane (Pr/Ph) ratios (Average 20.73, 0.61 respectively) and high hydrogen index (HI) (average 637.6) indicate that the formation was deposited under anoxic condition. According to regular sterane (C27%, C28%, C29%) and terpanes ratios (C29/C30, C31/C30 hopane), the formation was deposited in marine environment. |
topic |
chia gara formation, anoxic condition, biomarker assemblage type ii kerogen mature organic matter oil-prone |
url |
https://doi.org/10.1515/geo-2019-0007 |
work_keys_str_mv |
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_version_ |
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