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- W2353892495 abstract "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, hydrocarbon 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 20×108 t, which makes the basin a major target for hydrocarbon exploration in the South Yellow Sea." @default.
- W2353892495 created "2016-06-24" @default.
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- W2353892495 date "2010-01-01" @default.
- W2353892495 modified "2023-09-23" @default.
- W2353892495 title "Tectonic Evolution and Hydrocarbon Potential in Northern Area of the South Yellow Sea" @default.
- W2353892495 hasPublicationYear "2010" @default.
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