Affiliation:
1. School of Marine Sciences, Sun Yat-sen University, Guangzhou, 510275, China
2. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
Abstract
There are many previous studies on the formation mechanism of overpressure in sedimentary basins. The Yinggehai Basin is a typical strike-slip extensional basin with obvious overpressure phenomenon. Yinggehai Formation begins to appear overpressure in Central Diapir Zone with the depth of less than 2000 m. Undercompacted, hydrocarbon generation are the two main mechanisms for the formation of overpressure in Yinggehai Basin. Controlled by tectonic movements, Yinggehai Basin develops four kinds of structure-sedimentary patterns, and has a large deposition/subsidence rate formed thick mudstone layers. The thick mudstone layers not only form the undercompacted sedimentary background, also are good source rocks. Affected by Cenozoic lithospheric thinning, the Red River strike-slip fault activity and magmatic activity of local areas, Yinggehai Basin has high geo-temperature and high heat flow values which are conducive to hydrocarbon generation. This paper's study shows that tectonic movements control sedimentary facies types and distribution, deposition/subsidence rate, and geothermal field. Both of the two main mechanisms (undercompaction, hydrocarbon generation) of overpressure in Yinggehai Basin are all controlled by the tectonic movements. Therefore, the tectonic movements are the main controlling factor of overpressure formation in Yinggehai Basin.
Subject
Energy Engineering and Power Technology,Fuel Technology,Nuclear Energy and Engineering,Renewable Energy, Sustainability and the Environment
Reference41 articles.
1. 莺歌海盆地异常裂后沉降的动力学机制
2. Organic Matter Maturity and Clay Mineral Transformations in Overpressured Formations: Comparison Histories from Two Zones of the South Caspian Basin
3. Gong Z.S. and Li S.T., 1997. Dynamic Research of Oil and Gas Accumulation in the Northern Margin Basins of South China Sea. Beijing, Science Press. Pp. 63–126.
Cited by
2 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献