The origin and importance of Al₂SiO₅-bearing quartz veins in metamorphic rocks, with particular reference to the Amphibolite Facies
Metamorphosed pelitic rocks from the Eastern Dalradian (Scotland) contain Al₂SiO₅-bearing quartz veins. The veins formed during amphibolite-grade regional metamorphism. Veins occur in both Barrovian and Buchan-type terranes. Staurolite-grade pelitic schists in the Buchan region (Whitehills and Boynd...
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University of Derby
2007
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.486678 |