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PDF) The Pressure-Temperature Path and the Origin of Phlogopite in Spinel-Garnet Peridotites from the Blansky Les Massif of the Moldanubian Zone, Czech Republic
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The Pressure^Temperature Path and the Origin of Phlogopite in Spinel^Garnet Peridotites from the Blansky¤ Les Massif of the Mol
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Mantle processes in an Archean orogen: Evidence from 2.67 Ga diamond-bearing lamprophyres and xenoliths - ScienceDirect
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