The structural geology of the southern Norwegian Caledonides in the Oslo Graben and Sparagmite region
In order to construct the most continuous balanced cross-section from undeformed foreland to higher thrust sheets in the southern Caledonides of Norway, selected areas of Cambro-Silurian rocks were mapped in the Oslo Graben. Undeformed rocks are only present in the southern part of the Oslo Graben a...
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London Metropolitan University
1983
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.347408 |