Transition from oceanic to continental lithosphere subduction in southern Tibet: Evidence from the Late Cretaceous–Early Oligocene (~91–30 Ma) intrusive rocks in the Chanang–Zedong area, southern Gangdese

Transition from oceanic to continental lithosphere subduction in southern Tibet: Evidence from the Late Cretaceous–Early Oligocene (~91–30 Ma) intrusive rocks in the Chanang–Zedong area, southern Gangdese

Little is known about the detailed processes associated with the transition from oceanic to continental lithosphere subduction in the Gangdese Belt of southern Tibet (GBST). Here, we report zircon U–Pb age, major and trace element and Sr–Nd–Hf isotopic data for Late Cretaceous–Early Oligocene (~ 91–...

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Bibliographic Details
Main Authors: Jiang, Z., Wang, Qiang, Wyman, D., Li, Zheng-Xiang, Yang, J., Shi, X., Ma, L., Tang, G., Gou, G., Jia, X., Guo, H.
Format: Journal Article
Published: Elsevier BV 2014
Subjects:
Continental subduction - Southern Tibet
Slab breakoff
Adakites
Continental collision
Oceanic subduction
Online Access:http://hdl.handle.net/20.500.11937/6609

Internet

http://hdl.handle.net/20.500.11937/6609

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