A petrological and structural study of the Levang gneiss-dome, southern Norway
The Levang granite forms an elliptical body occupying the core of a broad antiformal structure, and covering approximately 50 sq. km. Surrounding this mass of granitoid gneisses is a series of banded gneisses of very variable composition, including amphibolites, quartzltes, and nodular sillimanite g...
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Durham University
1964
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.585704 |