LOSOS, Zdeněk and Miroslav BROŽ. Parageneze a chemismus bimetasomatických kontaktních zón žulovského masivu (Mineral assemblages and chemistry of the bimetasomatic contact zones from the Žulová massif). In Mineralogie Českého masivu a Západních Karpat. Olomouc: UP Olomouc, 2002, p. 59-62. Sborník referátů z mezinárodního semináře. ISBN 80-244-0454-0.
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Basic information
Original name Parageneze a chemismus bimetasomatických kontaktních zón žulovského masivu
Name (in English) Mineral assemblages and chemistry of the bimetasomatic contact zones from the Žulová massif
Authors LOSOS, Zdeněk (203 Czech Republic, guarantor) and Miroslav BROŽ (203 Czech Republic).
Edition Olomouc, Mineralogie Českého masivu a Západních Karpat, p. 59-62, Sborník referátů z mezinárodního semináře, 2002.
Publisher UP Olomouc
Other information
Original language Czech
Type of outcome Proceedings paper
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Czech Republic
Confidentiality degree is not subject to a state or trade secret
RIV identification code RIV/00216224:14310/02:00006255
Organization unit Faculty of Science
ISBN 80-244-0454-0
Keywords in English bimetasomatic contact zone; Žulová massif; pyroxen; garnet; P-T conditions; marble; gneiss
Tags bimetasomatic contact zone, garnet, gneiss, marble, P-T conditions, pyroxen, Žulová Massif
Changed by Changed by: doc. RNDr. Zdeněk Losos, CSc., učo 2470. Changed: 23/7/2002 11:15.
Abstract
Příspěvek shrnuje výsledky studia bimetasomatické kontaktní zóny, vyvinuté mezi mramory a pararulami v bezprostřední blízkosti granitoidů.
Abstract (in English)
The bimetasomatic contact zone between calcite marble and biotite gneiss located about 5 m from Žulová massif granite (locality Boží hora-old quarry) was studied. The contact zone with thickness about 20 cm is composed of the following subzones (the middle part of this contact zone /subzones 2b,2c/ are strongly silicified): 1) dark biotite gneiss /Plg,Bi,K-fs,Qtz/ with enormous enrichment of biotite, 2) bimetasomatic contact zone (2a- transformed gneiss rich in Cpx /Plg,Bi,Cpx/, 2b- Plg-Cpx-zone /Plg,Cpx,Grs,Qtz/, Plg is transformed into zoisite and prehnite, 2c- Grs-Hd-zone /Grs,Hd,Qtz/, 2d- Wo-zone /Wo,Ves,accessory Di/, 3) coarse-grained calcite marble /Cal, accessory Di,Qtz/.
Links
MSM 143100004, plan (intention)Name: Geologické procesy a jejich environmentální vyústění - styk variscid a alpid
Investor: Ministry of Education, Youth and Sports of the CR, Geological Processes and their Environmental Impact - Contact of the Variscides and Alpides
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