Field and petrographic evidence for partial melting of TTG gneiss within the central region of the mainland Lewisian complex, NW Scotland

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Field and petrographic evidence for partial melting of TTG gneiss within the central region of the mainland Lewisian complex, NW Scotland

The central region of the mainland Lewisian complex is dominated by granulite-facies tonalite–trondhjemite–granodiorite (TTG) gneisses that are highly depleted in some mobile trace elements (Cs, Rb, Th and U) relative to amphibolite-facies TTG gneisses elsewhere in the Lewisian complex and to the av...

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Bibliographic Details
Main Authors:	Johnson, Tim, Fischer, S., White, R.
Format:	Journal Article
Published:	Geological Society Publishing House 2013
Subjects:	migmatite Lewisian complex TTG gneiss partial melting field relations
Online Access:	http://hdl.handle.net/20.500.11937/3567

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