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Article: Organic geochemical characteristics of source rocks in Shoushangou Formation, Xi Ujimqin Banner of Inner Mongolia

TitleOrganic geochemical characteristics of source rocks in Shoushangou Formation, Xi Ujimqin Banner of Inner Mongolia
Authors
KeywordsKerogen types
Lower Permian
Maturity of organic matter
Organic matter abundance
Shoushangou Formation
Issue Date2013
Citation
Geological Bulletin of China, 2013, v. 32, n. 8, p. 1322-1328 How to Cite?
AbstractDark mudstone and shale of Lower Permian Shoushangou Formation are well developed in Xi Ujimqin Banner of Inner Mongolia. Organic geochemical studies of hydrocarbon source rock samples collected from Tabinmiao forestry center profile were conducted in the aspects of organic matter abundance, kerogen types and maturity of organic matter, so as to evaluate the hydrocarbon potential. Organic matter abundance of Shoushangou Formation in Xi Ujimqin Banner of Inner Mongolia has reached moderate to good hydrocarbon source rock standard; organic matter was derived mainly from higher plants, and the kerogen belongs to type III. Thermal evolution of organic matter entered into the mature to over mature stage. Hence the Shoushangou Formation is the potential hydrocarbon (particularly gas) source rock and serves as another important Upper Paleozoic layer in the peripheral oil and gas exploration of the Songliao basin.
Persistent Identifierhttp://hdl.handle.net/10722/327505
ISSN
2023 SCImago Journal Rankings: 0.262

 

DC FieldValueLanguage
dc.contributor.authorGong, Fan Hao-
dc.contributor.authorHuang, Xin-
dc.contributor.authorChen, Shu Wang-
dc.contributor.authorZheng, Yue Juan-
dc.contributor.authorZhang, Jian-
dc.contributor.authorSu, Fei-
dc.date.accessioned2023-03-31T05:31:51Z-
dc.date.available2023-03-31T05:31:51Z-
dc.date.issued2013-
dc.identifier.citationGeological Bulletin of China, 2013, v. 32, n. 8, p. 1322-1328-
dc.identifier.issn1671-2552-
dc.identifier.urihttp://hdl.handle.net/10722/327505-
dc.description.abstractDark mudstone and shale of Lower Permian Shoushangou Formation are well developed in Xi Ujimqin Banner of Inner Mongolia. Organic geochemical studies of hydrocarbon source rock samples collected from Tabinmiao forestry center profile were conducted in the aspects of organic matter abundance, kerogen types and maturity of organic matter, so as to evaluate the hydrocarbon potential. Organic matter abundance of Shoushangou Formation in Xi Ujimqin Banner of Inner Mongolia has reached moderate to good hydrocarbon source rock standard; organic matter was derived mainly from higher plants, and the kerogen belongs to type III. Thermal evolution of organic matter entered into the mature to over mature stage. Hence the Shoushangou Formation is the potential hydrocarbon (particularly gas) source rock and serves as another important Upper Paleozoic layer in the peripheral oil and gas exploration of the Songliao basin.-
dc.languageeng-
dc.relation.ispartofGeological Bulletin of China-
dc.subjectKerogen types-
dc.subjectLower Permian-
dc.subjectMaturity of organic matter-
dc.subjectOrganic matter abundance-
dc.subjectShoushangou Formation-
dc.titleOrganic geochemical characteristics of source rocks in Shoushangou Formation, Xi Ujimqin Banner of Inner Mongolia-
dc.typeArticle-
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.scopuseid_2-s2.0-84883799629-
dc.identifier.volume32-
dc.identifier.issue8-
dc.identifier.spage1322-
dc.identifier.epage1328-

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