Structural and chemical controls on melting in high grade metapelites, SW Finland
The Turku granulite terrain of southern Finland is located within the south-west corner of Svecofennian Schist Belt, part of the Scandinavian Svecofennian Orogenic Belt. The field area is a representative slice of an island arc system which collided against the northern Baltic Shield at 1890 Ma. Thi...
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University of Edinburgh
2000
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.663298 |