Reworking of the Gangdese magmatic arc, southeastern Tibet: post-collisional metamorphism and anatexis

The Gangdese magmatic arc, southeastern Tibet, was built by mantle‐derived magma accretion and juvenile crustal growth during the Mesozoic to Early Cenozoic northward subduction of the Neo‐Tethyan oceanic slab beneath the Eurasian continent. The petrological and geochronological data reveal that the...

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Veröffentlicht in:	Journal of metamorphic geology 2015-01, Vol.33 (1), p.1-21
Hauptverfasser:	Zhang, Z., Dong, X., Xiang, H., Ding, H., He, Z., Liou, J. G.
Format:	Artikel
Sprache:	eng
Schlagworte:	collisional orogenesis crustal reworking magmatic arc metamorphism south Tibet
Online-Zugang:	Volltext
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