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- W2373993869 abstract "Tianshan orogenic belt connects with the Tarim basin and Junggar basin from south to north respectively. Through a joint Paleozoic continental breakup,the South Tianshan Ocean and the North Tianshan ocean cracked,the continued expansion of ocean basins,oceanic crust subduction,continental collision and suture and Cenozoic tectonic adjustments,now it is the world's more active orogenic belt and become a domestic hot zone of continental dynamics. Based on comprehensive analysis of geological,geophysical(seismic profiles,gravity anomalies,seismic tomography),geochemical,petrological,and astronomy,etc.,combined with the tectonic evolution history of the Tianshan orogenic belt,the surface structural deformation,base tectonic style of the basin,and the deeply inquiry of the five kinds of mantle convection patterns,based on whole-mantle convection and small-scale upper mantle convection model,we propose that the dynamic mechanism of plate tectonic evolution coupled with the mantle convection in the Tianshan region totally presented as Start-Sync-Transcendence-Subtractive mode,and the middle course of the dynamic model with micro-oscillation cycle forward.This model can be compared with the classic Wilson cycle,while the current traces of the plate tectonic evolution in the deep crust and the numerical simulation of the mantle convection also supports this mode to some extent.In short of a unified dynamic model comhing the history and evolution of plate tectonics and mantle convectton,it will be of great significance for future study of coupling and interaction between all the subsystems of the Earth." @default.
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- W2373993869 date "2011-01-01" @default.
- W2373993869 modified "2023-09-27" @default.
- W2373993869 title "Coupling dynamic mechanisms between plate tectonics evolution and mantle convection of south and north Tianshan" @default.
- W2373993869 hasPublicationYear "2011" @default.
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