An experimental study of the breakdown of dolomite in H2O at 700 °C, 100 MPa
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DOI: 10.2138/am-2024-9368
Abstract: Abstract The occurrence of periclase in contact-metamorphosed dolomite rock at modest temperature and pressure indicates an infiltration of H2O because of the otherwise high temperature required for the reaction dolomite → periclase + calcite +… read more here.
Keywords: 100 mpa; h2o 700; breakdown dolomite; 700 100 ... See more keywords