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...
| Main Authors: | , , |
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| Format: | Journal Article |
| Published: |
Geological Society Publishing House
2013
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/3567 |