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The Dawros peridotite, Connemara, Eire

Quarterly Journal of the Geological Society of London, 1957
Summary The Dawros peridotites are characterized by a strong banding and evidence of thermal metamorphism exists in the enclosing schists. The banding arises from a rhythmic crystal accumulation ranging through a sequence of dunites and pyroxenites in which the assemblage olivine and orthopyroxene at one extreme passes into the assemblage ...
openaire   +1 more source

Spinel Peridotite

2013
Naresh Chandra Ghose   +2 more
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