Closed-system geochemical recycling of crustal materials in alpine-type peridotite
We examined aluminous mafic rock (with or without corundum or sapphirine) alternating with peridotite from the Ronda peridotite massif, southern Spain. On the basis of petrographic characteristics, these mafic rocks show a decompression history from high
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|Source:||Geochimica et Cosmochimica Acta|
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