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- W2358309747 abstract "A concept, diwa basin system of continental margin spreading type, has been put forward to express the crustobody evolutional-geodynamic environment of the exten-sional diwa basins distributed in the East Asia continental margin crustobody and formed in theresidual-mobility period of diwa stage. It has been pointed out that the genesis of the taphrogenic basins in the continental marginal sea diwa regions does not have relation to the ideal model of back- arc spreading caused by subduction of oceanic plates; and the basins do not belong to the Atlantic type. In-fact, the basins are results of extension and taph-rogeny of the continental crust that has evolved to the residual-mobility period of diwa stage and has undergone the Cathaysian diwa oro-gensis. An important mechanism, lower lithospheric delamination and extensional collapse of the Cathaysian diwa has been considered to explain the formation of the diwa basins of continental margin spreading type and a model has been built up to show the tectonic development from the Cathaysian diwa-type orogens to the basin-and-range-type structural zones, then to the continental marginal sea basins." @default.
- W2358309747 created "2016-06-24" @default.
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- W2358309747 date "1995-01-01" @default.
- W2358309747 modified "2023-09-28" @default.
- W2358309747 title "ON THE DIWA BASIN SYSTEM OF CONTINENTAL MARGIN SPREADING TYPE AND ITS GENETIC MECHANISM" @default.
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