Geochemistry of high grade gneisses, with examples from West Greenland and British Columbia
The ancient continental massifs of the world are typically composed of granulite grade met metamorphic rocks of calc-alkaline affinity. A model, based on experimental work, is derived to explain the processes by which the igneous precursors of the deep crustal gneisses were generated. It is suggeste...
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University of Leicester
1985
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.370673 |