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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
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SYSNO ASEP 0335101 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title The Pressure–Temperature Path and the Origin of Phlogopite in Spinel–Garnet Peridotites from the Blanský les Massif of the Moldanubian Zone, Czech Republic Author(s) Naemura, K. (JP)
Hirajima, T. (JP)
Svojtka, Martin (GLU-S) SAI, RID, ORCIDSource Title Journal of Petrology. - : Oxford University Press - ISSN 0022-3530
Roč. 50, č. 10 (2009), s. 1795-1827Number of pages 33 s. Publication form WWW - WWW Language eng - English Country GB - United Kingdom Keywords garnet ; metasomatism ; peridotite ; phlogopite ; P–T conditions Subject RIV DB - Geology ; Mineralogy CEZ AV0Z30130516 - GLU-S (2005-2011) UT WOS 000271577800001 EID SCOPUS 70349962938 DOI 10.1093/petrology/egp052 Annotation A new lithotype of peridotite, phlogopite- and apatite-bearing spinel–garnet peridotite, associated with leucocratic granulite, has been recognized at the Plešovice quarry in the Gföhl Unit within the Moldanubian Zone of the Bohemian Massif, Czech Republic. There are three equilibrium stages in the Pleovice peridotite. The existence of Stage I, the precursor spinel ± garnet peridotite stage, is supported by the presence of an aluminous (Al2O3 ~3,0 wt %) orthopyroxene megacryst in the matrix. The minimum temperature of Stage I was estimated to be 1020 ± 15°C. Workplace Institute of Geology Contact Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272 Year of Publishing 2010
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