Sedimentary and organic matter characteristics of Lower Cretaceous Jiufotang Formation in western Liaoning Province

CHEN Gang; ZHANG Xiaoming; YANG Guifang; HAN Gang; BIAN Jun; YANG Ya'nan; ZHUO Shengguang

doi:10.12097/gbc.dztb-38-2-3-426

Geological Bulletin of China > 2019 > 38(2-3): 426-436. > DOI: 10.12097/gbc.dztb-38-2-3-426

CHEN Gang, ZHANG Xiaoming, YANG Guifang, HAN Gang, BIAN Jun, YANG Ya'nan, ZHUO Shengguang. 2019: Sedimentary and organic matter characteristics of Lower Cretaceous Jiufotang Formation in western Liaoning Province. Geological Bulletin of China, 38(2-3): 426-436. DOI: 10.12097/gbc.dztb-38-2-3-426

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Sedimentary and organic matter characteristics of Lower Cretaceous Jiufotang Formation in western Liaoning Province

1.
Reseach Institute of Exploration and Development, PetroChina Jidong Oilfield Company, Tangshan 063004, Hebei, China
2.
Northeast Petroleum University at Qinhuangdao, Qinhuangao 066000, Hebei, China
3.
China University of Petroleum, Beijing 102249, China
4.
Northeast University at Qinhuangdao, Qinhuangdao 066004, Hebei, China

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Received Date: December 04, 2017
Revised Date: April 15, 2018
Available Online: August 15, 2023

Graphical Abstract

Abstract

Abstract

Lower Cretaceous Jiufotang Formation is one of the important source rock stratigraphic horizon in Mesozoic strata of western Liaoning Province. It is widespread in Jianchang-Kazuo Basin, with thickness of 206~2118m, but is relatively thinner in Fuxin-Yixian Basin. Organic geochemistry analyses indicate the two basins have both developed good to excellent source rocks characterized by good kerogen type and low maturity. The second section of Jiufotang Formation, which was formed in flunctuating profundal facies, is optimistic source rock horizon with average TOC of 9.5% and kerogen ofⅠtype. The first and third sections of Jiufotang Formation, which were formed in fluvial-lacustrine facies, have relatively poor source rock development environment due to shallower water body. The biomarkers analyses indicate that source rocks in the second section of Jiufotang Formation were developed in a clay-rich reducing brackish lake. The preliminary genetic analysis indicates that the development of these source rocks was attributed to good conservation condition from chemical stratification of lake water body and relatively high primary production.
- western Liaoing Province,
- Jiufotang Formation,
- source rocks evaluation,
- Lower Cretaceous

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References (32)

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Sedimentary and organic matter characteristics of Lower Cretaceous Jiufotang Formation in western Liaoning Province