Late Cretaceous (100–89 Ma) magnesian charnockites with adakitic affinities in the Milin area, eastern Gangdese: Partial melting of subducted oceanic crust and implications for crustal growth in southern Tibet

Late Cretaceous (100–89 Ma) magnesian charnockites with adakitic affinities in the Milin area, eastern Gangdese: Partial melting of subducted oceanic crust and implications for crustal growth in southern Tibet

Rapid Mesozoic–Early Cenozoic crustal growth in the Gangdese area, southern Tibet, has commonly been, attributed to pre-collisional and syn-collisional underplating of mantle-derived magmas. Here, we report on, adakitic magnesian charnockites (i.e., hypersthene-bearing diorites and granodiorites) ne...

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Bibliographic Details
Main Authors: Ma, L., Wang, Qiang, Wyman, D., Li, Zheng-Xiang, Jiang, Z., Yang, J., Gou, G., Guo, H.
Format: Journal Article
Published: Elsevier BV 2013
Subjects:
Crust growth
Slab melting
Tibet
Adakitic charnockite
Gangdese batholith
Roll-back
Online Access:http://hdl.handle.net/20.500.11937/5393

Internet

http://hdl.handle.net/20.500.11937/5393

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