断陷盆地海陆过渡相烃源岩发育模式:以西湖凹陷平湖组为例

田杨; 叶加仁; 雷闯; 吴克强; 刘一茗

doi:10.3799/dqkx.2018.940

Volume 44 Issue 3

Mar. 2019

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Article Navigation > Earth Science > 2019 > 44(3): 898-908

Tian Yang, Ye Jiaren, Lei Chuang, Wu Keqiang, Liu Yiming, 2019. Development Model for Source Rock of Marine-Continental Transitional Face in Faulted Basins: A Case Study of Pinghu Formation in Xihu Sag. Earth Science, 44(3): 898-908. doi: 10.3799/dqkx.2018.940

Citation:

Tian Yang, Ye Jiaren, Lei Chuang, Wu Keqiang, Liu Yiming, 2019. Development Model for Source Rock of Marine-Continental Transitional Face in Faulted Basins: A Case Study of Pinghu Formation in Xihu Sag. Earth Science, 44(3): 898-908. doi: 10.3799/dqkx.2018.940

Citation:

Tian Yang, Ye Jiaren, Lei Chuang, Wu Keqiang, Liu Yiming, 2019. Development Model for Source Rock of Marine-Continental Transitional Face in Faulted Basins: A Case Study of Pinghu Formation in Xihu Sag. Earth Science, 44(3): 898-908. doi: 10.3799/dqkx.2018.940

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Development Model for Source Rock of Marine-Continental Transitional Face in Faulted Basins: A Case Study of Pinghu Formation in Xihu Sag

doi: 10.3799/dqkx.2018.940

Tian Yang^{1,2
,},
Ye Jiaren^{2
,
,},
Lei Chuang³,
Wu Keqiang⁴,
Liu Yiming²

1.
Hubei Cooperative Innovation Center of Unconventional Oil and Gas, Yangtze University, Wuhan 430100, China
2.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
College of Mining Engineering, North China University of Science and Technology, Tangshan 063210, China
4.
CNOOC Research Institute Ltd., Beijing 100028, China

Received Date: 2018-12-26
Publish Date: 2019-03-15

Abstract

Abstract

Source rock in Pinghu Formation of Eocene is the main source rock series in Xihu hydrocarbon generating sag of the East China Sea shelf basin, and it is also a typical source rock of marine-continental transitional face in the faulted basins of East China.Using drilling, seismic data combined with organic geochemistry and paleontology data of hydrocarbon source rock, the development controlling factors for the Pinghu Formation are discussed and the forming model is established by analyses of characteristics of the hydrocarbon source rock and tectonic-sedimentary-palaeoclimate development background in this study.It is found that source rocks in Pinghu Formation of Xihu Sag are characterized by wide distribution, large thickness and multiple series of thin coal seam with carbonaceous mudstone, relatively high quality of source rocks.The development background of Pinghu Formation is a semi-enclosed bay environment with warm-humid subtropical climate condition, and predominantly terrestrial organic matter contribution.The development of hydrocarbon source rocks in Pinghu Formation is mainly affected by sedimentation-subsidence rate, source material and preservation condition of organic matter, forming model could be concluded with "rapid subsidence, warm-humid climate, terrestrial organic matter, fresh-brackish water, and relatively strong oxidation condition".
- Pinghu Formation,
- marine-continental transitional face,
- source rock,
- controlling factors,
- forming model,
- Xihu Sag,
- petroleum geology

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References(62)

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Development Model for Source Rock of Marine-Continental Transitional Face in Faulted Basins: A Case Study of Pinghu Formation in Xihu Sag

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