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The Pressure–Temperature Path and the Origin of Phlogopite in Spinel–Garnet Peridotites from the Blanský les Massif of the Moldanubian Zone, Czech Republic
- 1.NAEMURA, K., HIRAJIMA, T., SVOJTKA, M. The Pressure–Temperature Path and the Origin of Phlogopite in Spinel–Garnet Peridotites from the Blanský les Massif of the Moldanubian Zone, Czech Republic. Journal of Petrology. 2009, 50(10), 1795-1827. ISSN 0022-3530. E-ISSN 1460-2415. Available: doi: 10.1093/petrology/egp052
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