Add to ORKGSiliceous duricrusts are distributed in regions of the Czech Republic largely as scattered solitary boulders, except ones from north-west Bohemia. Two genetic categories have been recognized: pedogenic and groundwater silcrete. Their division is based on description of micromorphology under polarizing/scanning electron microscopy, analysis of major oxides chemistry by ICP together with composition of individual micromorphological features by electron microprobe
Foraminifera of the Lower Badenian Brno Sands of the Carpathian Foredeep from the TGB-1 Borehole nea...
The bimodal spilite-keratophyre association in the Konice-Mladeč Belt is poor in acid rocks. A small...
Siliceous and opal coatings and impregnations were found to form surface hardening forms on the surf...
The tectonic development of the northern part of Moravian Karst can be divided into three phases at ...
The complex slope failure at Vaculov Sedlo is located about 8 km north-east of Vsetín (E Moravia). ...
In its early history the polygenetic depression of the Upper Moravia Graben (UMG) evolved in two sep...
The Rača Unit of the Magura Nappe in the Hostýn Hills is composed of siliciclastics ranging in age f...
Silesian Unit represents a good example of fully developed turbidite (flysch) basin, where it is par...
Petrographic study of the Lower Carboniferous sediments at the map sheet 25-123 Hranice proved diffe...
In the SE surroundings of the Great Moravian site Břeclav-Pohansko the occurrences of aeolian sands ...
In karst valley stream Říčky we can find these sorts of caves: karst springs, through caves, swallow...
Several relics of a 4045 m terrace are preserved in the area east of the Pavlovské vrchy Hills. They...
The present article summarizes the main works dealing with the Jaslo Shales of the Menilite-Krosno S...
The influence of structural pattern and stratigraphic relations on karstification of Upper Devonian ...
The clay mineral identification in fine fraction of slope sediments of five individual landslides in...
Foraminifera of the Lower Badenian Brno Sands of the Carpathian Foredeep from the TGB-1 Borehole nea...
The bimodal spilite-keratophyre association in the Konice-Mladeč Belt is poor in acid rocks. A small...
Siliceous and opal coatings and impregnations were found to form surface hardening forms on the surf...
The tectonic development of the northern part of Moravian Karst can be divided into three phases at ...
The complex slope failure at Vaculov Sedlo is located about 8 km north-east of Vsetín (E Moravia). ...
In its early history the polygenetic depression of the Upper Moravia Graben (UMG) evolved in two sep...
The Rača Unit of the Magura Nappe in the Hostýn Hills is composed of siliciclastics ranging in age f...
Silesian Unit represents a good example of fully developed turbidite (flysch) basin, where it is par...
Petrographic study of the Lower Carboniferous sediments at the map sheet 25-123 Hranice proved diffe...
In the SE surroundings of the Great Moravian site Břeclav-Pohansko the occurrences of aeolian sands ...
In karst valley stream Říčky we can find these sorts of caves: karst springs, through caves, swallow...
Several relics of a 4045 m terrace are preserved in the area east of the Pavlovské vrchy Hills. They...
The present article summarizes the main works dealing with the Jaslo Shales of the Menilite-Krosno S...
The influence of structural pattern and stratigraphic relations on karstification of Upper Devonian ...
The clay mineral identification in fine fraction of slope sediments of five individual landslides in...
Foraminifera of the Lower Badenian Brno Sands of the Carpathian Foredeep from the TGB-1 Borehole nea...
The bimodal spilite-keratophyre association in the Konice-Mladeč Belt is poor in acid rocks. A small...
Siliceous and opal coatings and impregnations were found to form surface hardening forms on the surf...