Late Permian-Triassic magmatic evolution in the Jinshajiang orogenic belt, SW China and implications for orogenic processes following closure of the Paleo-Tethys

Late Permian-Triassic magmatic evolution in the Jinshajiang orogenic belt, SW China and implications for orogenic processes following closure of the Paleo-Tethys

Growth of continental crust involves the complex interplay of subduction zone magmatism, to generate the crust, followed by stabilization through crustal thickening, magmatism and ultimately isolation from the active plate margin. The Jinshajiang orogenic belt, SW China, provides an exceptional reco...

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Bibliographic Details
Main Authors: Zi, Jianwei, Cawood, P., Fan, W., Tohver, E., Wang, Y., McCuaig, T., Peng, T.
Format: Journal Article
Published: American Journal of Science 2013
Subjects:
Jinshajiang orogenic belt
Ludian batholith
magmatic evolution
closure of Paleo-Tethys
Online Access:http://hdl.handle.net/20.500.11937/17263

Internet

http://hdl.handle.net/20.500.11937/17263

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