Pan-African granulites of Madagascar and southern India: Gondwana assembly and parallels with modern Tibet

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Pan-African granulites of Madagascar and southern India: Gondwana assembly and parallels with modern Tibet

Granulites of the southern East African Orogen formed by continental collision during Gondwana assembly. The highest metamorphic gradients of 25-50°C km-1 were attained at 0.58-0.53 Ga in a microcontinental block that was sandwiched between two collisional sutures and is now exposed in Madagascar an...

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Bibliographic Details
Main Author:	Fitzsimons, Ian
Format:	Journal Article
Published:	Japan Association of Mineralogical Sciences 2016
Online Access:	http://hdl.handle.net/20.500.11937/36237

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