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From Dolerite to Diorite: Older Granite Activity near Ellon, Aberdeenshire
Published online by Cambridge University Press: 01 May 2009
Abstract
Hornblende-schists, probably intruded as dolerite sills, have been permeated by trondhjemitic material. Conversion to rocks of dioritic aspect is the end-stage of this process, but the intermediate stages are more common. The conversion has been effected with little displacement so that all varieties can be observed in their correct sequence.
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