Organic geochemical characteristics of Jurassic Yan ’an Formation source rock in Pengyang area of southwestern Ordos basin

The Jurassic Yan ’an Formation in the southwestern margin of Ordos Basin has developed many sets of coal-associated and non-associated mudstone as well as oil shale. Different analytical methods including total organic carbon (TOC), Rock-Eval pyrolysis, and conventional biomarker analyses were appli...

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Main Authors: Yaling Zhu, Wenmei Tan, Lianfu Hai, Caixia Mu, Kun Wang, Mengyuan Li
Format: Article
Language:English
Published: Frontiers Media S.A. 2025-02-01
Series:Frontiers in Earth Science
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Online Access:https://www.frontiersin.org/articles/10.3389/feart.2025.1536268/full
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author Yaling Zhu
Yaling Zhu
Wenmei Tan
Lianfu Hai
Lianfu Hai
Caixia Mu
Caixia Mu
Kun Wang
Mengyuan Li
author_facet Yaling Zhu
Yaling Zhu
Wenmei Tan
Lianfu Hai
Lianfu Hai
Caixia Mu
Caixia Mu
Kun Wang
Mengyuan Li
author_sort Yaling Zhu
collection DOAJ
description The Jurassic Yan ’an Formation in the southwestern margin of Ordos Basin has developed many sets of coal-associated and non-associated mudstone as well as oil shale. Different analytical methods including total organic carbon (TOC), Rock-Eval pyrolysis, and conventional biomarker analyses were applied on the mudstone, the coal and the oil shale extracts to unravel their organic geochemical characteristics and the paleo depositional environment. Results reveal that all the source rock samples are immature to mature with good petroleum generation potentials. The redox environment is generally reducing. The organic matter input is mainly terrestrial higher plants. The low Ga/C30 hopane ratio of all the samples indicate the low salinity of the paleo-water column. The oil shale samples show much higher thermal maturity than the coals and mudstones as indicated by the higher C31 homohopane isomerization indexes, C32 homohopane isomerization indexes and the C29 sterane ααα20S/(S + R) ratios. The depositional environment of the oil shale is more reduced compared to the coals and mudstones as can be reflected by the low oxygen index and the higher C35 hopane/(C31-C35 homohopanes) ratios. Thus, the oil shale layers should be the target of the next exploration and development. And the Oil shale and coal can be exploited simultaneously in Pengyang area.
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publishDate 2025-02-01
publisher Frontiers Media S.A.
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spelling doaj-art-d1b46f0d3a0a44d69ab319a9a3cdcf0f2025-02-04T06:31:47ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632025-02-011310.3389/feart.2025.15362681536268Organic geochemical characteristics of Jurassic Yan ’an Formation source rock in Pengyang area of southwestern Ordos basinYaling Zhu0Yaling Zhu1Wenmei Tan2Lianfu Hai3Lianfu Hai4Caixia Mu5Caixia Mu6Kun Wang7Mengyuan Li8School of Geosciences, Yangtze University, Wuhan, ChinaHubei Key Laboratory of Complex Shale Oil and Gas Geology and Development in Southern China, Wuhan, ChinaSchool of Geosciences, Yangtze University, Wuhan, ChinaMineral Geological Survey Institute of Ningxia Hui Autonomous Region, Yinchuan, ChinaInstitute of Mineral Geology of Ningxia Hui Autonomous Region, Yinchuan, ChinaMineral Geological Survey Institute of Ningxia Hui Autonomous Region, Yinchuan, ChinaInstitute of Mineral Geology of Ningxia Hui Autonomous Region, Yinchuan, ChinaSchool of Geosciences, Yangtze University, Wuhan, ChinaSchool of Geosciences, Yangtze University, Wuhan, ChinaThe Jurassic Yan ’an Formation in the southwestern margin of Ordos Basin has developed many sets of coal-associated and non-associated mudstone as well as oil shale. Different analytical methods including total organic carbon (TOC), Rock-Eval pyrolysis, and conventional biomarker analyses were applied on the mudstone, the coal and the oil shale extracts to unravel their organic geochemical characteristics and the paleo depositional environment. Results reveal that all the source rock samples are immature to mature with good petroleum generation potentials. The redox environment is generally reducing. The organic matter input is mainly terrestrial higher plants. The low Ga/C30 hopane ratio of all the samples indicate the low salinity of the paleo-water column. The oil shale samples show much higher thermal maturity than the coals and mudstones as indicated by the higher C31 homohopane isomerization indexes, C32 homohopane isomerization indexes and the C29 sterane ααα20S/(S + R) ratios. The depositional environment of the oil shale is more reduced compared to the coals and mudstones as can be reflected by the low oxygen index and the higher C35 hopane/(C31-C35 homohopanes) ratios. Thus, the oil shale layers should be the target of the next exploration and development. And the Oil shale and coal can be exploited simultaneously in Pengyang area.https://www.frontiersin.org/articles/10.3389/feart.2025.1536268/fullOrdos basinYan ’an Formationsource rocksbiomarkeroil shale
spellingShingle Yaling Zhu
Yaling Zhu
Wenmei Tan
Lianfu Hai
Lianfu Hai
Caixia Mu
Caixia Mu
Kun Wang
Mengyuan Li
Organic geochemical characteristics of Jurassic Yan ’an Formation source rock in Pengyang area of southwestern Ordos basin
Frontiers in Earth Science
Ordos basin
Yan ’an Formation
source rocks
biomarker
oil shale
title Organic geochemical characteristics of Jurassic Yan ’an Formation source rock in Pengyang area of southwestern Ordos basin
title_full Organic geochemical characteristics of Jurassic Yan ’an Formation source rock in Pengyang area of southwestern Ordos basin
title_fullStr Organic geochemical characteristics of Jurassic Yan ’an Formation source rock in Pengyang area of southwestern Ordos basin
title_full_unstemmed Organic geochemical characteristics of Jurassic Yan ’an Formation source rock in Pengyang area of southwestern Ordos basin
title_short Organic geochemical characteristics of Jurassic Yan ’an Formation source rock in Pengyang area of southwestern Ordos basin
title_sort organic geochemical characteristics of jurassic yan an formation source rock in pengyang area of southwestern ordos basin
topic Ordos basin
Yan ’an Formation
source rocks
biomarker
oil shale
url https://www.frontiersin.org/articles/10.3389/feart.2025.1536268/full
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