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《Geotectonica Et Metallogenia》 2004-02
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GENETIC MECHANISMS OF MUD-FLUID DIAPIR IN YINGGEHAI BASIN AND HYDROCARBON ACCUMULATION

ZHANG Minqiang~1, ZHONG Zhihong~1, XIA Bin~1, LI Xuxuan~1, SUN Zhen~2, WANG Liangshu~3 and Wang Zhenfeng~4 (1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2. South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, GD 510301, China; 3. The Department of Earth Sciences, Nanjing University, Nanjing, JS 210093, China; 4. Nanhai West Corporation, CNOOC, Zhanjiang, GD 524057, China)  
The evolution of mud-fluid diapir in Yinggehai Basin is the result of regional stress field variation and (over-pressure) system formation and evolution. Development of the over-pressure system is caused by disequilibrium compaction and thermal evolution that are intimately related to the structural styles of the basin. Variation of the regional stress field resulted in the mud-diapirism in mid-Miocene and the fluid diapirism in late Miocene to Quaternary. The structures formed during the early mud-diapirism stage obviously controlled the later stage fluid diapirism. For the shallow traps in Yinggehai Formation, the main reason for episodic injection of fluid with different gas components is the matching of trap formation and hydrocarbon generation in Miocene.
【Fund】: 中国科学院知识创新项目 (编号KZCX2 SW 117 0 2 )的部分成果
【CateGory Index】: P618.13
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