Publication Date:
1953-12-01
Description:
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.
Print ISSN:
0016-7568
Electronic ISSN:
1469-5081
Topics:
Geosciences
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