北塘凹陷古近系烃源岩特征及热演化史模拟

白云风; 王华; 王振升; 廖远涛; 林正良; 黄传炎

doi:10.3799/dqkx.2011.057

Volume 36 Issue 3

May 2011

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Article Navigation > Earth Science > 2011 > 36(3): 565-571

BAI Yun-feng, WANG Hua, WANG Zhen-sheng, LIAO Yuan-tao, LIN Zheng-liang, HUANG Chuan-yan, 2011. Thermal Evolution Modeling and Characteristic of Source Rock of Paleogene in Beitang Sag. Earth Science, 36(3): 565-571. doi: 10.3799/dqkx.2011.057

Citation:

BAI Yun-feng, WANG Hua, WANG Zhen-sheng, LIAO Yuan-tao, LIN Zheng-liang, HUANG Chuan-yan, 2011. Thermal Evolution Modeling and Characteristic of Source Rock of Paleogene in Beitang Sag. Earth Science, 36(3): 565-571. doi: 10.3799/dqkx.2011.057

Citation:

BAI Yun-feng, WANG Hua, WANG Zhen-sheng, LIAO Yuan-tao, LIN Zheng-liang, HUANG Chuan-yan, 2011. Thermal Evolution Modeling and Characteristic of Source Rock of Paleogene in Beitang Sag. Earth Science, 36(3): 565-571. doi: 10.3799/dqkx.2011.057

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Thermal Evolution Modeling and Characteristic of Source Rock of Paleogene in Beitang Sag

doi: 10.3799/dqkx.2011.057

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
E & D Research Institute of Daqing Oilfield Company Ltd., Daqing 163712, China
3.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
4.
E & D Research Institute of Dagang Oilfield Company Ltd., CNPC, Dagang 300280, China

Received Date: 2010-12-28
Publish Date: 2011-05-01

Abstract

Abstract

Based on large quantity of organic geochemistry data, the geochemistry characteristics are systematically analyzed on organic carbonate content (TOC), chloroform bitumen "A", overall hydrocarbon content, S₁+S₂, organic matter types and maturity (R_o%) and so on. It shows that the Dong 3 Member, Sha 1 Member and Sha 3 Member are the main oil source beds of Beitang sag, especially, Sha 3 Member is the best in source rock quality. The model results indicate that (1) The depth of oil generative threshold is about 2 390 m, and the temperature is about 94.2℃, and the time entering on the oil generative threshold is from 25 Ma to 28 Ma in Beitang sag; (2) The present-day temperature of Sha 3 Layer is 140-160℃, the present-day R_o ranges between 0.9%-1.4%, It is in its peak of oil generation. The temperature of Sha 1+2 Layer is 100-140℃, the R_o ranged between 0.75%-1.0%, which suggests that it is in the middle-maturity at present. The present-day temperature of Dongying Layer is 80-100℃, the present-day R_o ranges between 0.45%-0.75%, which indicates that the present-day source rocks are in low maturation.
- Beitang sag,
- Paleogene,
- source rock,
- thermal evolution history modeling,
- sedimentology

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References(39)

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Thermal Evolution Modeling and Characteristic of Source Rock of Paleogene in Beitang Sag

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