The emplacement and deformation of granitic rocks in a transpressional shear zone : the Ox Mountains igneous complex
The structural evolution of the Ox Mountains Granodiorite (478±12Ma) during and after its emplacement is described. This pluton has been emplaced within and synchronously with, a major transpressional shear zone which is expressed as a 11km wide belt of strongly deformed NE-SW striking, steeply dipp...
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Durham University
1989
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.252665 |