Record details

Title
    Magnetic fabric and weak deformation in sandstones of accretionary prisms of the Flysch and Klippen Belts of the Western Carpathians: Mostly offscraping indicated
Author
    Hrouda, František
    Krejci, Oldrich
    Potfaj, Michal
    Stranik, Zdenek
Language
    anglicky
Publication type
    článek v periodiku
Source title - serial
    TECTONOPHYSICS
Vol./nr.
    Roč. 479, č. 3-4
Pages
    15
Year
    2009
Thesaurus term
    Accreationary prism
    Flysch Belt of the Western Carpathians
    Magnetic fabric
Keyword
    Accretionary
    Belts
    Carpathians
    Deformation
    Fabric
    Flysch
    Indicated
    Klippen
    Magnetic
    Mostly
    Offscraping
    Prisms
    Sandstones
    Weak
    Western
Abstract (in english)
   The magnetic fabric of sandstones in thrust sheets of the Flysch Belt of the Western Carpathians is basically sedimentary in origin, in minority of specimens slightly affected by deformation which is generally very weak, corresponding to the earliest deformation stage and to Types I-II in terms of the magnetic fabric classification of the accretionary prisms by Pares et al. (1999) and Aubourg et al. (2004), respectively. This indicates an absence of the return flow during the subduction process.
Contributor
    UK Praha, Přírodovědecká fakulta
Contributor code
    UK, PřF
Source format
    R
Import date
    8. 8. 2012