The Mšeno-Roudnice Coal Basin is an eastern part of the Central Bohemian Carboniferous Coal Basins. The total thickness of the Carboniferous sediments is ranging from several tens of metres in the south up to nearly 1 km in the basin centre. The basin was explored by nearly 55 deep boreholes with the aim to explore coal reserves. The seismic exploration in the basin has been carried out, too. Fossil stream pattern was reconstructed, of which rivers eroded the upper part of the Slaný Formation sediments during the intra-Stephanian hiatus between the Slaný and Líně Formation (Stephanian B/C). The project could have been realized due to some drilling close to seismic profiles, and also at least due to locally favourable seismological condition...
The Upper Silesian Coal Basin (USCB) represents a typical foreland basin developed during the Varisc...
The Donets Basin (Donbas) is one of the major late Paleozoic coal basins in the world. The Donbas Fo...
Geological boundaries of the structural stages between Late Variscan Moravian-Silesian-Cracow orogen...
The Ostrava-Karvina coalfield represents the Czechoslovak part of the Upper Silesian Basin, which is...
Líně Formation is the youngest basin fill unit of the Upper Palaeozoic Central and Western Bohemian ...
Angular coal clasts confined to coarse-grained feldspathic sandstone deposited in the Tuchlovice Min...
Abstract: In 1994 research in the Czech Republic began into coalbed methane (CBM). The target of thi...
The deep boreholes in the Upper Silesian Coal Basin provide a valuable material to evaluate thermal ...
Tyt. z nagłówka.Art. jest abstr. referatu z konferencji.Bibliogr. s. 117.The Upper Carboniferous coa...
Coal clast in upper carboniferous sediments in the Czech part of Upper Silesian Coal Basin - sedimen...
Borehole no Stonava SV 2 was realized in 1968 - 70 yrs. for the verification of the stratigraphy of...
In the submitted article the authors express their view on some present trends in the assessment o...
© SGEM2016.The Volga-Ural oil and gas province is located in the eastern part of the East European p...
This article aims to explain and demonstrate the origin and development of a subsidence basin caused...
The Petřkovice Member is the basal unit of the paralic succession of the Ostrava Formation of the Up...
The Upper Silesian Coal Basin (USCB) represents a typical foreland basin developed during the Varisc...
The Donets Basin (Donbas) is one of the major late Paleozoic coal basins in the world. The Donbas Fo...
Geological boundaries of the structural stages between Late Variscan Moravian-Silesian-Cracow orogen...
The Ostrava-Karvina coalfield represents the Czechoslovak part of the Upper Silesian Basin, which is...
Líně Formation is the youngest basin fill unit of the Upper Palaeozoic Central and Western Bohemian ...
Angular coal clasts confined to coarse-grained feldspathic sandstone deposited in the Tuchlovice Min...
Abstract: In 1994 research in the Czech Republic began into coalbed methane (CBM). The target of thi...
The deep boreholes in the Upper Silesian Coal Basin provide a valuable material to evaluate thermal ...
Tyt. z nagłówka.Art. jest abstr. referatu z konferencji.Bibliogr. s. 117.The Upper Carboniferous coa...
Coal clast in upper carboniferous sediments in the Czech part of Upper Silesian Coal Basin - sedimen...
Borehole no Stonava SV 2 was realized in 1968 - 70 yrs. for the verification of the stratigraphy of...
In the submitted article the authors express their view on some present trends in the assessment o...
© SGEM2016.The Volga-Ural oil and gas province is located in the eastern part of the East European p...
This article aims to explain and demonstrate the origin and development of a subsidence basin caused...
The Petřkovice Member is the basal unit of the paralic succession of the Ostrava Formation of the Up...
The Upper Silesian Coal Basin (USCB) represents a typical foreland basin developed during the Varisc...
The Donets Basin (Donbas) is one of the major late Paleozoic coal basins in the world. The Donbas Fo...
Geological boundaries of the structural stages between Late Variscan Moravian-Silesian-Cracow orogen...