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Tectonic Evolution and Hydrocarbon Potential in Northern Area of the South Yellow Sea 被引量:6
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作者 姚永坚 陈春峰 +3 位作者 冯志强 张拭颖 郝天珧 万荣胜 《Journal of Earth Science》 SCIE CAS CSCD 2010年第1期71-82,共12页
The northern area of the South Yellow Sea, located in the offshore region of China, resulted from the continental-continental collision orogeny during the Mesozoic and can be divided into four stages in terms of tecto... The northern area of the South Yellow Sea, located in the offshore region of China, resulted from the continental-continental collision orogeny during the Mesozoic and can be divided into four stages in terms of tectonic evolution: (1) pre-orogenic passive continental margin stage (Z-T2); (2) foreland basin stage corresponding with the late phase of the Sulu (苏鲁) orogeny (J3-K); (3) post-orogenic intracontinental rifted basin stage (K2t-E); and (4) regional subsidence and coverage stage (N-Q). Based on detailed investigation and study of the intracontinental rifted basin, hydrocar- bon source rocks of Late Cretaceous Taizhou (泰州) Formation distributed well in the basin, and four reservoir-cap combinations as well as numerous trap structures were found. As a result, the geological conditions would be excellent for reservoir formation in the basin, and the oil resource amount is estimated at about 20×10^8 t, which makes the basin a major target for hydrocarbon exploration in the South Yellow Sea. 展开更多
关键词 northern area of the South Yellow Sea tectonic evolution stage OROGENY source- reservoir-cap combination hydrocarbon exploration potential.
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