Three outcrops of the Lower Badenian marginal sediments Kletná, Stachovice (near Suchdol nad Odrou) and Střítež nad Ludinou (near Hranice) have been documented by sedimentological, petrological and micropaleontological methods. The coarse-grained sandstones and fine-grained conglomerates with clasts of metamorphosed rocks, Culmian sediments and quartz pebbles prevail in the studiying profiles. Two lithofacies were recognised in the outcrop Kletná: Gt – channel fill conglomerates; Gh – horizontally laminate conglomerates. Only one lithofacie Gi – very coarse sandstones to granules with layers of medium-grained conglomerates – was found on the locality Stachovice. Lithofacies Gt and Gm documenting amalgamated conglomerate beds were described ...
This text is focused mainly on landslide-affected clays and clayey soils taken from the Brno-Medlánk...
There was studied the infilling of a sunken house from Modřice near Brno, dated to the Hallstatt per...
The medieval crucibles from two localities – Brno, Mečová Street and Jihlava Staré Hory were studied...
The fluvial deposits of the Paleo-Svratka River were studied on 3 localities in the broader surround...
The eastern part of the Bohemian Massif consists of many geological crystalline complexes with diffe...
The structure of the Pavlov Hills was formed during folding and thrusting within the Outer Carpathia...
The Kelč facies of the Silesian Unit represents slope sediments – mostly shale (mudstones). Carbon a...
Studied locality Choryně is situated in the Silesian Unit of the Outer Western Carpathian’s flysch. ...
The amphibolites from the Vícenice quarry are part of a larger body on the northwestern margin of th...
Dome-like hills are broadly distributed in both studied areas. Southwest of Krnov these hills, rarel...
In the frontal part of the Bílé Karpaty Unit the Upper Cretaceous sediments of the Antonínek Formati...
Heavy minerals represent a good tool for determination of the source area of stream sediments. Studi...
Cretaceous silicious sandstones, limestones and claystones mostly as pebbles in the topsoil were det...
Artificial lakes and reservoirs serve as traps for suspended sediment. In this paper we study sedime...
The paper is dealing with geological setting of the Bílé Karpaty Unit (Magura Flysch Group of nappes...
This text is focused mainly on landslide-affected clays and clayey soils taken from the Brno-Medlánk...
There was studied the infilling of a sunken house from Modřice near Brno, dated to the Hallstatt per...
The medieval crucibles from two localities – Brno, Mečová Street and Jihlava Staré Hory were studied...
The fluvial deposits of the Paleo-Svratka River were studied on 3 localities in the broader surround...
The eastern part of the Bohemian Massif consists of many geological crystalline complexes with diffe...
The structure of the Pavlov Hills was formed during folding and thrusting within the Outer Carpathia...
The Kelč facies of the Silesian Unit represents slope sediments – mostly shale (mudstones). Carbon a...
Studied locality Choryně is situated in the Silesian Unit of the Outer Western Carpathian’s flysch. ...
The amphibolites from the Vícenice quarry are part of a larger body on the northwestern margin of th...
Dome-like hills are broadly distributed in both studied areas. Southwest of Krnov these hills, rarel...
In the frontal part of the Bílé Karpaty Unit the Upper Cretaceous sediments of the Antonínek Formati...
Heavy minerals represent a good tool for determination of the source area of stream sediments. Studi...
Cretaceous silicious sandstones, limestones and claystones mostly as pebbles in the topsoil were det...
Artificial lakes and reservoirs serve as traps for suspended sediment. In this paper we study sedime...
The paper is dealing with geological setting of the Bílé Karpaty Unit (Magura Flysch Group of nappes...
This text is focused mainly on landslide-affected clays and clayey soils taken from the Brno-Medlánk...
There was studied the infilling of a sunken house from Modřice near Brno, dated to the Hallstatt per...
The medieval crucibles from two localities – Brno, Mečová Street and Jihlava Staré Hory were studied...