. "35"^^ . . "2" . "The Lahn-Dill type deposit of Mal\u00FD D\u011Bd 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 Mal\u00FD D\u011Bd deposit occurs in close association with muscovite-biotite gneiss of the Precambrian Desn\u00E1 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." . . . "Fojt, Bohuslav" . . "RIV/00216224:14310/10:00056592" . "14310" . . "M\u00FCcke, Arno" . "Petrography, mineralogy, geochemistry and genetic aspects of the Lahn-Dill type deposit of Mal\u00FD D\u011Bd (=Leiterberg) in the Devonian Vrbno Group (Silesicum), Czech Republic"@en . . "Vrbno Group; Silesicum; Lahn-Dill; petrography-petrology; fluid inclusions; microscopy; mineral chemistry; ankerite-dolomite solid solution; whole rock geochemistry; genesis"@en . . "95" . . . . "1211-8796" . . . . . "Petrography, mineralogy, geochemistry and genetic aspects of the Lahn-Dill type deposit of Mal\u00FD D\u011Bd (=Leiterberg) in the Devonian Vrbno Group (Silesicum), Czech Republic" . . "[1C29119D4B37]" . . "Doln\u00ED\u010Dek, Zden\u011Bk" . "1"^^ . "Acta Musei Moraviae, Scientiae geologicae" . "S" . "3"^^ . "CZ - \u010Cesk\u00E1 republika" . "Petrography, mineralogy, geochemistry and genetic aspects of the Lahn-Dill type deposit of Mal\u00FD D\u011Bd (=Leiterberg) in the Devonian Vrbno Group (Silesicum), Czech Republic" . . "Petrography, mineralogy, geochemistry and genetic aspects of the Lahn-Dill type deposit of Mal\u00FD D\u011Bd (=Leiterberg) in the Devonian Vrbno Group (Silesicum), Czech Republic"@en . . "278677" . "The Lahn-Dill type deposit of Mal\u00FD D\u011Bd 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 Mal\u00FD D\u011Bd deposit occurs in close association with muscovite-biotite gneiss of the Precambrian Desn\u00E1 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."@en . "RIV/00216224:14310/10:00056592!RIV12-MSM-14310___" . . .