Record details

Title
    The Mšeno-Roudnice basin : problems of reconstruction of fossil stream pattern (Central Bohemian Coal Basins, Czech Republic)
Statement of responsibility
    Jiří Skopec, Jiří Pešek, Miroslav Kobr
Other titles
    Proceedings of the IV European Coal Conference, September 26-28, 2000, Ustroń, Poland (Variant.)
Author
    Kobr, Miroslav, 1940-
    Pešek, Jiří, 1936-
    Skopec, Jiří
Language
    anglicky
Source title - serial
    Polish geological institute special papers
Vol./nr.
    Vol. 7
Pages
    p. 229-236
Year
    2002
Notes
    6 obr.
    il.
    Obsahuje bibliografické odkazy
    Zkr. název ser.: Pol. geol. Inst. spec. Pap.
Classfication no.
    55(1)
    550.8
    551.7
    553.9
Conspectus category
    55
    553
Subject group
    karbon-svrchní
    karotáž gama
    mšensko-roudnická pánev
    paleoreliéf
    profil seizmický
    sedimentace fluviální
    stefan
    středočeské svrchní paleozoikum
    uhlí bituminózní
Geographical name
    ČR-Čechy
    Mšeno (Mělník, Mělník)
    Roudnice nad Labem (Litoměřice, Roudnice nad Labem)
Keyword
    Basin
    Basins
    Bohemian
    Central
    Coal
    Czech
    Fossil
    Mšeno-Roudnice
    Pattern
    Problems
    Reconstruction
    Republic
    Stream
Abstract (in english)
   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 conditions. The results allowed to decipher the anomalous depositional structure of the Slany and Line formations that was difficult to be defined earlier.
   The results showed that some tectonic movements occurred towards the end of the Stephanian B which resulted in giving rise of erosional activity of ancient streams
Contributor
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
    U
Entered date
    27. 11. 2008
Import date
    8. 8. 2012