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Sr-sulphate and associated minerals found from kyanite-bearing eclogite in the Moldanubian Zone of the Bohemian Massif, Czech Republic
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SYSNO ASEP 0350018 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Sr-sulphate and associated minerals found from kyanite-bearing eclogite in the Moldanubian Zone of the Bohemian Massif, Czech Republic Tvůrce(i) Nakamura, D. (JP)
Kobayshi, T. (JP)
Shimobayashi, N. (JP)
Svojtka, Martin (GLU-S) SAI, RID, ORCID
Hirajima, T. (JP)Zdroj.dok. Journal of Mineralogical and Petrological Sciences. - : Japan Association of Mineralogical Sciences - ISSN 1345-6296
Roč. 105, č. 5 (2010), s. 251-261Poč.str. 11 s. Forma vydání WWW - WWW Jazyk dok. eng - angličtina Země vyd. JP - Japonsko Klíč. slova celestine ; Sr ; eclogite ; sulphide ; Bohemian Massif Vědní obor RIV DB - Geologie a mineralogie CEZ AV0Z30130516 - GLU-S (2005-2011) UT WOS 000283959000002 EID SCOPUS 78649616690 DOI 10.2465/jmps.090817 Anotace Sr-bearing phase, celestine (SrSO4), was found in ultrahigh-pressure (UHP) eclogite associated with the Nové Dvory peridotite mass in the Moldanubian Zone of the Bohemian Massif, Czech Republic. Celestine is closely associated with anhydrite (CaSO4) and sulphides; pyrite, pyrrhotite and chalcopyrite. Fe-rich unknown silicate mineral developing along the margin of the sulphide minerals was also found. Those minerals in the eclogite occur in the matrix that is mainly occupied with fine-grained clinopyroxene aggregate. A common Sr reservoir in eclogite is known to be epidote, but the maximum pressure-temperature (P-T) conditions of the studied eclogite was estimated as about 1000–1100°C, 4.5–4.9 GPa. In such extremely high P-T conditions, epidote should be unstable. In fact, epidote is absent from most of eclogites in the Moldanubian Zone of Czech Republic. Pracoviště Geologický ústav Kontakt Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272 Rok sběru 2011
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