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- W2378164497 abstract "Xingkai taphrogenesis of South China plate in Neoproterozoic began in Jinning movement(800 MaB.C.),and ended in Yu'nan movement in Middle Ordovician(458 Ma B.C.),the strong activity occurring inmid-Neoproterozoic Suxiong-Kaijianqiao formation volcanic eruption(700 Ma B.C.).The evolution happened atthe time when the disintegration of Rodinia super-continent,and was part of breakup Rodinia.It formed the baseof Yangtze in Xingkai taphrogenesis,and had an important effect on tectonic deformation to middle-upper Yangtzeregion.It provided the base of large uplift and depression in Caledonian,and formed basement faults that hadcontrol action to Sichuan basin,and provided conditions of source rock in Low Paleozoic with formed stable continentalmargin.So it is of the great significance in petroleum exploration to research the characteristics of Xingkaitaphrogenesis in Sichuan basin and middle-upper Yangtze region." @default.
- W2378164497 created "2016-06-24" @default.
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- W2378164497 date "2011-01-01" @default.
- W2378164497 modified "2023-09-27" @default.
- W2378164497 title "CHARACTERISTICS OF XINGKAI TAPHROGENESIS IN SOUTH CHINA AND THE EFFECTSON OIL AND GAS" @default.
- W2378164497 hasPublicationYear "2011" @default.
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