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The Dunites in the Balmuccia peridotite massif.
2007The Balmuccia massif is dominantly lherzolitic. Dunites are a minor lithotype occurring: a) at the contacts of websterite dykes; b) as tabular bodies associated with layers of Cr-rich spinel; c) as large, decametric lenses typically associated with hornblendite pockets and veins. Type a dunites are 15 cm), olivine coexists with clinopyroxene.
RIVALENTI, Giorgio +5 more
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THE ORTHOPYROXENE-GARNET GEOBAROMETER FOR PERIDOTITES
International Geology Review, 1990N. P. Androsenko +4 more
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A Primary Peridotite Magma-Revisited: Olivine Quench Crystals in a Peridotite Lava
1972openaire +2 more sources