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
![Mantle processes in an Archean orogen: Evidence from 2.67 Ga diamond-bearing lamprophyres and xenoliths - ScienceDirect Mantle processes in an Archean orogen: Evidence from 2.67 Ga diamond-bearing lamprophyres and xenoliths - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0024493706000235-gr2.jpg)
Mantle processes in an Archean orogen: Evidence from 2.67 Ga diamond-bearing lamprophyres and xenoliths - ScienceDirect
![Mantle processes in an Archean orogen: Evidence from 2.67 Ga diamond-bearing lamprophyres and xenoliths - ScienceDirect Mantle processes in an Archean orogen: Evidence from 2.67 Ga diamond-bearing lamprophyres and xenoliths - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0024493706000235-gr4.jpg)
Mantle processes in an Archean orogen: Evidence from 2.67 Ga diamond-bearing lamprophyres and xenoliths - ScienceDirect
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PDF) Microdiamond in a low-grade metapelite from a Cretaceous subduction complex, western Kyushu, Japan
![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 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](https://www.researchgate.net/profile/Martin-Svojtka/publication/31230370/figure/fig1/AS:668971200159749@1536506571293/a-Geotectonic-subdivisions-of-the-Variscan-orogenic-belt-in-central-Europe-Cooke_Q320.jpg)
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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