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- W2377462210 abstract "The Wanan Basin in Nansha area is a rifting basin located in the passive marin of the SW subbasin of the South China Sea. Through the characteristics of geophysical field and the distribution of faults, especially by interpretation of seismic profiles and contrdsting well data, we compared and interpreted seven reflected interfases, Tl, T2, T3, T4, T5, T6 and Tg, of which Tg, T5 and T3 represent three regional unconfondties and are the reflections of three tectonic movements in the Cenozoic sediments of Wanan Basin. According to the three regional unconformities the Cenozoic sediments can be subdivided into three tectonic layers: Tg-T5, T5-T3 and T3- seafloor. Therefore, we infer that there were three tectonic movements in Cenozoic in the Wanan Basin. So the tectonic evolutional history has experienced three phases: The Shenghu Movement (the end of Cretaceous-early Paleocene), the Nanhai Movement (lato Eocene- early Oligocene) and the Wanan Movement The Period from Shenghu Movement to Nanhai Movement was the foundational Phase while the Period from Nanhai Movement to Wanan Movement was the development phase in Wanan Basin. From the Wanan Movement to the present the regional subsidence in Wanan Basin occurred, which is the formation phase of Wanan Basin.The tectonic evolutional history of the Wanan Basin experienced three tectonic movements and three development phases, and is similar to the eastern part of the Zhujiang River Mouth Basin, so that we infer that there should exist rich oil and gasresources in the Wanan Basin." @default.
- W2377462210 created "2016-06-24" @default.
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- W2377462210 date "1997-01-01" @default.
- W2377462210 modified "2023-09-28" @default.
- W2377462210 title "A REDISCUSSION ON THE TECTONIC EVOLUTIONAL HISTORY OF THE WANAN BASIN IN NANSHA AREA" @default.
- W2377462210 hasPublicationYear "1997" @default.
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