Post-collisional Ultrapotassic Mafic Magmatism in South Tibet: Products of Partial Melting of Pyroxenite in the Mantle Wedge Induced by Roll-back and Delamination of the Subducted Indian Continental Lithosphere Slab

Post-collisional (25-8 Ma) ultrapotassic mafic magmatic rocks occur to the north of the India-Asia collision zone within the Lhasa terrane of the southern Tibetan Plateau, forming a near 1000 km long semi-continuous igneous belt. They include both extrusive and intrusive facies, although lava flows...

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Veröffentlicht in:	Journal of petrology 2015-07, Vol.56 (7), p.1365-1406
Hauptverfasser:	Guo, Zhengfu, Wilson, Marjorie, Zhang, Maoliang, Cheng, Zhihui, Zhang, Lihong
Format:	Artikel
Sprache:	eng
Schlagworte:	Crusts Magma Mantle Melting Rocks Slabs Tibet Wedges
Online-Zugang:	Volltext
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