Carbonation of peridotites and decarbonation of siliceous dolomites represented in the system CaO-MgO-SiO2-CO2 to 30 kbar
作者： P.J. Wyllie , W.-L. Huang , Jens Otto , A.P. Byrnes
DOI: 10.1016/0040-1951(83)90194-4
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摘要: The decarbonation of siliceous dolomite produces rocks including the minerals forsterite, orthopyroxene and clinopyroxene, characteristic of peridotites. Selected reactions in the system …
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