MÜCKE, Arno, Bohuslav FOJT and Zdeněk DOLNÍČEK. Petrography, mineralogy, geochemistry and genetic aspects of the Lahn-Dill type deposit of Malý Děd (=Leiterberg) in the Devonian Vrbno Group (Silesicum), Czech Republic. Acta Musei Moraviae, Scientiae geologicae. Brno: Moravské zemské muzeum, vol. 95, No 2, p. 95-129. ISSN 1211-8796. 2010.
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Basic information
Original name Petrography, mineralogy, geochemistry and genetic aspects of the Lahn-Dill type deposit of Malý Děd (=Leiterberg) in the Devonian Vrbno Group (Silesicum), Czech Republic
Name in Czech Petrografie, mineralogie, geochemie a genetické aspekty ložiska typu lahn-dill Malý Děd (=Leiterberg) v devonské Vrbenské skupině (Silesikum), Česká republika
Authors MÜCKE, Arno (276 Germany), Bohuslav FOJT (203 Czech Republic, guarantor, belonging to the institution) and Zdeněk DOLNÍČEK (203 Czech Republic).
Edition Acta Musei Moraviae, Scientiae geologicae, Brno, Moravské zemské muzeum, 2010, 1211-8796.
Other information
Original language English
Type of outcome Article in a journal
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/00216224:14310/10:00056592
Organization unit Faculty of Science
Keywords (in Czech) Vrbenská skupina; Silesikum; lahn-dill; petrografie- petrologie; fluidní inkluze; mikroskopie; genéza
Keywords in English Vrbno Group; Silesicum; Lahn-Dill; petrography-petrology; fluid inclusions; microscopy; mineral chemistry; ankerite-dolomite solid solution; whole rock geochemistry; genesis
Tags AKb, rivok
Changed by Changed by: Mgr. Tomáš Marhanský, učo 356572. Changed: 29/3/2012 11:56.
Abstract
The Lahn-Dill type deposit of Malý Děd located in the Silesian domain is a part of the Devonian metasedimentary and metavolcanic cover rocks (Vrbno Group) that contain about 30 small Lahn-Dill typeiron-ore occurences. The Malý Děd deposit occurs in close association with muscovite-biotite gneiss of the Precambrian Desná Dome. The investigations involved detailed petrographic-petrological studies supported by whole-rock geochemical, mineral (amphibole, biotite, chlorite, carbonate, feldspar, magnetite and ilmenite) and fluid inclusion studies.
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