Overpressure in moderately deep to deep strata in the Lengjia-Leijia area,western Liaohe Depression,Bohai Bay Basin:Origin and effects on hydrocarbon accumulation

被引:0
|
作者
Chen C. [1 ,2 ]
Qiu N. [1 ]
Gao R. [2 ]
Zhou X. [2 ]
Sun Y. [3 ]
Yang L. [4 ]
Fu J. [4 ]
机构
[1] College of Geosciences, China University of Petroleum(Beijing), Beijing
[2] Research Institute of Exploration and Development, Liaohe Oilfield Company, PetroChina, Liaoning, Panjin
[3] School of petroleum engineering, Chongqing University of Science & Technology, Chongqing
[4] School of Earth Sciences, Northeast Petroleum University, Heilongjiang, Daqing
来源
Oil and Gas Geology | 2024年 / 45卷 / 01期
关键词
accumulation mode; genetic mechanism; Lengjia-Leijia area; Liaohe Depression; moderately deep to deep strata; overpressure;
D O I
10.11743/ogg20240109
中图分类号
学科分类号
摘要
The moderately deep to deep strata in the Lengjia-Leijia area,western Liaohe Depression exhibit significant overpressure. It’s of great significance to understanding its genetic mechanism and its effects on hydrocarbon migration and accumulation in terms of hydrocarbon exploration therein. Based on measured formation pressure and temperature,log data,and structural analysis,we comprehensively investigate the characteristics and genetic mechanisms of overpressure in these strata and explore its role in hydrocarbon accumulation therein. The results indicate that the Lengjia-Leijia area is characterized by composite thermo-pressure system of the overpressure,normal-pressure,and underpressure types,with the overpressure interval predominantly found in the 3rd and 4th members of the Shahejie Formation(also referred to as the Sha 3 Member and the Sha 4 Member,respectively)within the sub-sag zone,at depths ranging from 2 500 to 4 000 m approximately. The overpressure in the area primarily results from undercompaction,followed by a combination of hydrocarbon generation-induced pressurization,diagenesis,and tectonic compression. There exist two major hydrocarbon migration and accumulation modes in the study area:the self-sourced indigenous mode within overpressure zones and the cross-pressure mode from an overpressure zone to a normal-pressure/underpressure zone. The former is predominantly found within the overpressure zones of the Sha 3 and 4 members in the sub-sag zone. In contrast,the latter occurred during the period of faulting,including overpressure-driven hydrocarbon charging into the Leijia and Gaosheng structural zones from source rocks in the Sha 4 Member in the Chenjia sub-sag,and hydrocarbon accumulation in the eastern steep slope area and Xinglongtai buried hill in the Lengjia area after transporting through faults and sand bodies from the overpressure zones in the lower to middle sub-members of the Sha 3 Member. © 2024 Editorial Department of Oil and Gas Geology. All rights reserved.
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页码:130 / 141
页数:11
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