The tectonic evolution of mantle rocks from the Lizard Ophiolite Complex, south-west England
In SW England, a highly deformed and metamorphosed assemblage of ultramafic, mafic and granitic rocks is interpreted to represent a fragment of upper mantle and lower oceanic crust: the Lizard Ophiolite Complex. Although the processes involved in the tectonic and chemical evolution of mafic rocks an...
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Durham University
1999
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.298582 |