The Laxford shear zone: an end-Archaean terrane boundary?
The Lewisian Gneiss Complex of northwestern Scotland consists of Archaean gneisses, variably reworked during the Proterozoic. It can be divided into three districts – a central granulitefacies district between districts of amphibolite-facies gneiss to the north and south. Recent work has interprete...
| Main Authors: | , , , , , , , , , , |
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| Other Authors: | |
| Format: | Journal Article |
| Published: |
Geological Society Publishing House
2010
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| Online Access: | http://hdl.handle.net/20.500.11937/17611 |