Record details

Title
    Magnetic fabric and weak deformation in sandstones of accretionary prism of the Flysch and Klippen Belts of the Western Carpathians: Mostly offscraping indicated
Author
    Hrouda, František
    Krejčí, Oldřich
    Potfaj, Michal
    Stráník, Zdeněk
Language
    anglicky
Publication type
    článek v periodiku
Source title - serial
    Tectonophysics
Vol./nr.
    Roč. 479, č. 3-4
Pages
    17
Year
    2009
Thesaurus term
    magnetic fabric, Carpathian Flysch, Mesozoic, Palaeogene, structural geology, geodynamical evolution
Keyword
    Accretionary
    Belts
    Carpathians
    Deformation
    Fabric
    Flysch
    Indicated
    Klippen
    Magnetic
    Mostly
    Offscraping
    Prism
    Sandstones
    Weak
    Western
Abstract (in english)
   The deformation is weaker in the Bílé Karpaty and Oravská Magura thrust sheets in the East than in the Fore-Magura, Rača and Bystrica thrust sheets that are located in the centre of the Flysch Belt. In the Ždánice and Silesian sheets, the weak defromation reflects their sedimentation on the European slope of the Flysch belt basin and relatively short transport during their thrusting over the Foredeep.
Contributor
    Česká geologická služba
Contributor code
    ČGS (RIV)
Source format
    R
Import date
    15. 10. 2014