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Petrography, mineralogy, geochemistry and genetic aspects of the Lahn-Dill type deposit of Malý Děd (=Leiterberg) in the Devonian Vrbno Group (Silesicum), Czech Republic

MÜCKE, Arno, Bohuslav FOJT and Zdeněk DOLNÍČEK

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

Language

English

Type of outcome

Článek v odborném periodiku

Field of Study

10500 1.5. Earth and related environmental sciences

Country of publisher

Czech Republic

Confidentiality degree

není předmětem státního či obchodního tajemství

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

Změněno: 29/3/2012 11:56, Mgr. Tomáš Marhanský

Abstract

V originále

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.