Podrobnosti záznamu

Název
    Geometry of fold arrays in the Silesian-Cracovian region of southern Poland
Údaj o odpovědnosti
    Leslaw Teper
Další názvy
    Forces Folds and Fractures (Variant.)
Autor
    Teper, Leslaw
Jazyk
    anglicky
Zdrojový dokument - seriál
    Geological society special publication
Svazek/č.
    Vol. 169
Strany
    p. 167-179
Rok
    2000
Poznámky
    14 obr., 2 s.bibl.
    il.
    Zkr. název ser.: Geol. Soc. spec. Publ. (London).
Předmětová skupina
    anomálie tíhová
    geometrie
    hornoslezská pánev
    karbon-svrchní
    kinematika
    mapa strukturní
    uhelná sloj
    uhelný revír
    vrása
    vrásnění variské
    zóna střižná
Geografické jméno
    ČR-Morava
    Ostrava
    Polsko
Klíčové slovo
    Arrays
    Fold
    Geometry
    Poland
    Region
    Silesian-Cracovian
    Southern
Abstrakt (anglicky)
   A zone of deformation characterized by en echelon folds extends along the northeast margin of the Upper Silesian Coal basin in southern Poland. The zone is well exposed by mining in numerous colliers where the deformation involving Uppe Carboniferous strata can be observed. Folds and associated faults form a structural pattern consistent with an origin in dextral convergent wrenching on both the principal deep-seated fractures and the subsidiary faults affecting crystalline basement beneath this part of the basin. The zone is cross-cut by subblatitudinal fold belts which, according to their geometrical parameters, seem to result from alternate transcurrent shearing along west-east oriented fractures in the basement, sinistral in one case and dextral in the other.
   Among folds caused by the coficentrated operation of a force couple whose vectros lie in the horizontal plane, there are examples of bending folds (forced folds) in each array resulting from vertical components of movement of deep-seated fault blocks. The dimensions of the folds change with depth, and the axial trend and the inclination of axial surfaces differ with distance from the basement fault trace. The length of fold segments strongly depends on axes orientation. Widely distributed evidence of interlayer slip demonstrates a variable spatial distribution of tectonic-transport direction in the sedimentary sequence
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    25. 3. 2008
Datum importu
    8. 8. 2012