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The Dawros peridotite, Connemara, Eire
Quarterly Journal of the Geological Society of London, 1957Summary 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 ...
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The roles of pyroxenite and peridotite in the mantle sources of oceanic basalts
, 2017A. Matzen, B. Wood, M. Baker, E. Stolper
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Nickel–cobalt contents of olivine record origins of mantle peridotite and related rocks
, 2016C. Herzberg, C. Vidito, N. Starkey
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