The bimodal spilite-keratophyre association in the Konice-Mladeč Belt is poor in acid rocks. A small body of acid volcanites occurs at Ludmírov. Petrographically these rocks correspond to alkali feldspar rhyolite. The studied rocks contain phenocrysts of Kfeldspar, quartz and albite in a fine-grained groundmass composed mainly of quartz and K-feldspar; the proportion of albite in the groundmass is very small. Monazite-(Ce), rutile and zircon are accessory minerals
Palaeozoic (Devonian and Lower Carboniferous) rocks together with its Proterozoic basement are expos...
The influence of structural pattern and stratigraphic relations on karstification of Upper Devonian ...
Hydrothermal fluorite mineralization is located within hydrothermally altered pegmatites near Rakšic...
Epigenetic manganese ores (about 40 wt % MnO2 tot.) form up to eight cm thick hard horizon found in ...
The Rača Unit of the Magura Nappe in the Hostýn Hills is composed of siliciclastics ranging in age f...
Tourmaline forms needle – like aggregates in quartzite in the deposit Zlaté Hory – West („Mír“ galle...
Petrographic study of the Lower Carboniferous sediments at the map sheet 25-123 Hranice proved diffe...
In its early history the polygenetic depression of the Upper Moravia Graben (UMG) evolved in two sep...
In this paper there are described the litology and petrology of the Pústevny and Malinovská skála Sa...
In the Rača Unit of the Magura group of nappes the Ráztoka Beds of the Soláň Formation were studied ...
Siliceous duricrusts are distributed in regions of the Czech Republic largely as scattered solitary ...
Garnets from biotite and amphibole-biotite gneisses of the Rožná uranium deposit are part of grossul...
The paper brinks a description of a few small granitoid outcrops (the Olomouc Massif) in the Upper M...
The Oskava volcano-sedimentary complex of the Devonian age hosts sulfide mineralization of the SEDEX...
Variscan hydrothermal calcite±quartz veins have been investigated by microthermometric and isotopic ...
Palaeozoic (Devonian and Lower Carboniferous) rocks together with its Proterozoic basement are expos...
The influence of structural pattern and stratigraphic relations on karstification of Upper Devonian ...
Hydrothermal fluorite mineralization is located within hydrothermally altered pegmatites near Rakšic...
Epigenetic manganese ores (about 40 wt % MnO2 tot.) form up to eight cm thick hard horizon found in ...
The Rača Unit of the Magura Nappe in the Hostýn Hills is composed of siliciclastics ranging in age f...
Tourmaline forms needle – like aggregates in quartzite in the deposit Zlaté Hory – West („Mír“ galle...
Petrographic study of the Lower Carboniferous sediments at the map sheet 25-123 Hranice proved diffe...
In its early history the polygenetic depression of the Upper Moravia Graben (UMG) evolved in two sep...
In this paper there are described the litology and petrology of the Pústevny and Malinovská skála Sa...
In the Rača Unit of the Magura group of nappes the Ráztoka Beds of the Soláň Formation were studied ...
Siliceous duricrusts are distributed in regions of the Czech Republic largely as scattered solitary ...
Garnets from biotite and amphibole-biotite gneisses of the Rožná uranium deposit are part of grossul...
The paper brinks a description of a few small granitoid outcrops (the Olomouc Massif) in the Upper M...
The Oskava volcano-sedimentary complex of the Devonian age hosts sulfide mineralization of the SEDEX...
Variscan hydrothermal calcite±quartz veins have been investigated by microthermometric and isotopic ...
Palaeozoic (Devonian and Lower Carboniferous) rocks together with its Proterozoic basement are expos...
The influence of structural pattern and stratigraphic relations on karstification of Upper Devonian ...
Hydrothermal fluorite mineralization is located within hydrothermally altered pegmatites near Rakšic...