The geology of the Belhelvie mafic intrusion and its environs, Aberdeenshire
The Belhelvie mass has been remapped using shallow level drilling and interpretation of a detailed magnetic survey to augment outcrop mapping: this has shown the existence of the following sequence of rock units (west to east). a thin noritic zone (150 m. thick) serpentinized dunitic peridotite troc...
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University of Aberdeen
1972
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.592156 |