Podrobnosti záznamu

Název
    Apparent contradiction between tectonics and deposition in overturned strata - a case study from the "Moravian Culm" (Czech Republic)
Autor
    Havíř, Josef
    Otava, Jiří
Jazyk
    anglicky
Typ dokumentu
    článek v periodiku
Zdrojový dokument - seriál
    Geological Quarterly
Svazek/č.
    Roč. 50, č. 3
Strany
    4
Rok
    2006
Výraz tezauru
    Culm facies
    slumping
    stratigraphical polarity
    Variscan folding
Klíčové slovo
    Apparent
    Case
    Contradiction
    Culm
    Czech
    Deposition
    Moravian
    Overturned
    Republic
    Strata
    Study
    Tectonics
Abstrakt (anglicky)
   An apparent contradiction between structural and sedimentological indications commonly used for discrimination of the overturned and non-overturned beds during geological mapping was found at Paršovice, a site situated in the easternmost part of the European Variscides. This outcrop of folded Lower Carboniferous siliciclastic rocks of the "Culm facies" lies on the NE margin of the Bohemian Massif, in the SE part of the Maleník Block (Moravia, Czech Republic). At the same site, a slump-related isoclinal fold was found. The apparent contradiction between structural (relation of cleavage and bedding) and sedimentological (flute casts on bed soles) indications is explained by a combination of successive phases of slump- and tectonically-related folding.
Přispěvatel
    MU Brno, Přírodovědecká fakulta
Kód přispěvatele
    MU, PřF
Zdrojový formát
    R
Datum importu
    8. 8. 2012