鄂西-渝东地区下侏罗统东岳庙段泥岩地球化学特征及有机质富集模式

郭来源; 张士万; 解习农; 李忠生; 黄传炎; 陈北辰

doi:10.3799/dqkx.2017.100

Volume 42 Issue 7

Jul. 2017

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Article Navigation > Earth Science > 2017 > 42(7): 1235-1246

Guo Laiyuan, Zhang Shiwan, Xie Xinong, Li Zhongsheng, Huang Chuanyan, Chen Beichen, 2017. Geochemical Characteristics and Organic Matter Enrichment of the Dongyuemiao Member Mudstone of Lower Jurassic in the Western Hubei-Eastern Chongqing. Earth Science, 42(7): 1235-1246. doi: 10.3799/dqkx.2017.100

Citation:

Guo Laiyuan, Zhang Shiwan, Xie Xinong, Li Zhongsheng, Huang Chuanyan, Chen Beichen, 2017. Geochemical Characteristics and Organic Matter Enrichment of the Dongyuemiao Member Mudstone of Lower Jurassic in the Western Hubei-Eastern Chongqing. Earth Science, 42(7): 1235-1246. doi: 10.3799/dqkx.2017.100

Citation:

Guo Laiyuan, Zhang Shiwan, Xie Xinong, Li Zhongsheng, Huang Chuanyan, Chen Beichen, 2017. Geochemical Characteristics and Organic Matter Enrichment of the Dongyuemiao Member Mudstone of Lower Jurassic in the Western Hubei-Eastern Chongqing. Earth Science, 42(7): 1235-1246. doi: 10.3799/dqkx.2017.100

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Geochemical Characteristics and Organic Matter Enrichment of the Dongyuemiao Member Mudstone of Lower Jurassic in the Western Hubei-Eastern Chongqing

doi: 10.3799/dqkx.2017.100

1.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Exploration and Development Research Institute of Jianghan Oilfield Branch Company of SINOPEC, Wuhan 430079, China
3.
Division of Earth Science and Resource Engineering of CSIRO, Sydney

Received Date: 2017-02-10
Publish Date: 2017-07-15

Abstract

Abstract

The shale heterogeneity in different regions of China is the basic geological issue to be addressed urgently. However, the study of continental shale gas in the Sichuan basin is very weak. Based on analysis of the petrology and geochemistry of the Dongyuemiao member of lower Jurassic Ziliujing Formation in western Hubei-eastern Chongqing area, and combined with the logging curve, the vertical variation of geochemical characteristics and organic matter enrichment have been discussed. The results show that the Dongyuemiao member has high brittle mineral content and low clay mineral content, and higher organic matter content at the lower part than that at the upper part. Geochemical index, such as paleoclimate, paleoproductivity, paleoredox, paleosalinity has obvious vertical differences in the Dongyuemiao member. The lower part of Dongyuemiao member shows dry paleoclimate, dysoxic water column, saline water and high paleoproductivity, but the upper part of Dongyuemiao member shows warm and humid paleoclimate, low salination water and low paleoproductivity. It is concluded that the lower part of Dongyuemiao member has been more favourable for organic matter enrichment.
- western Hubei-eastern Chongqing area,
- mudstone,
- Dongyuemiao member,
- geochemistry,
- sedimentary environment,
- petroleum geology

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References(74)

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Geochemical Characteristics and Organic Matter Enrichment of the Dongyuemiao Member Mudstone of Lower Jurassic in the Western Hubei-Eastern Chongqing

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