Parageneze a chemismus bimetasomatických kontaktních zón žulovského masivu
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 | |
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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 | |
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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 |
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Příspěvek shrnuje výsledky studia bimetasomatické kontaktní zóny, vyvinuté mezi mramory a pararulami v bezprostřední blízkosti granitoidů. |
Abstract (in English) |
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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/. |
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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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