Podrobnosti záznamu

Název
    Westernmost occurrence of the Middle Miocene Badenian gypsum in central Paratethys (Kobeřice, Moravia, Czech Republic). Evaporite Formations of the carpathians Mts.. Part I. - Badenian
Údaj o odpovědnosti
    Tadeusz Marek Peryt, Stanislav Karoli, Danuta Peryt, Oleg I. Petričenko, Przemyslaw Gedl, Wanda Narkiewicz, Jarmila Ďurkovičová, Zofia Dobieszynska
Autor
    Dobieszynska, Zofia
    Ďurkovičová, Jarmila
    Gedl, Przemyslaw
    Karoli, Stanislav
    Narkiewicz, Wanda
    Peryt, Danuta
    Peryt, Tadeusz Marek
    Petričenko, Oleg I.
Jazyk
    anglicky
Zdrojový dokument - seriál
    Slovak geological magazine
Svazek/č.
    Vol. 3, no. 2
Strany
    p. 105-120
Rok
    1997
Poznámky
    6 obr., 2 s.bibl.
    Anglické resumé
    Zkr. název ser.: Slov. geol. Mag.
Předmětová skupina
    inkluze fluidní
    izotopy stabilní
    karpatská neogenní předhlubeň
    ložisko sádrovce
    mikrofosílie
    miocén-střední
    Paratethys
    sádrovec
    sedimentologie
Geografické jméno
    ČR-Morava
    Kobeřice (Opava)
Klíčové slovo
    Badenian
    Carpathians
    Central
    Czech
    Evaporite
    Formations
    Gypsum
    Kobeřice
    Middle
    Miocene
    Moravia
    Mts
    Occurrence
    Paratethys
    Republic
    Westernmost
Abstrakt (anglicky)
   The gypsum sequence outcropping in an active gypsum quarry in Kobeřice shows many similarities to other sections know from the northern marginal part of the Badenian basin. However, the pecularities of Kobeřice gypsum section indicate its more basinward localiton when compared to other gypsum exposures known from Poland and West Ukraine. The lower part consists of crystalline gypsum (giant gypsum intergrowths, sabre gypsum) accompanied by gypsiferous claystones and microcrystalline gypsum, and the upper part consists of interbedded laminated gypsum, gypsiferous claystones and breccias. These breccias are interpreted as debrites. The laminated gypsum units can be interpreted as fall-out from a low-density turbid layer. The major part of the gypsum sequence of Koběřice originated thus in deeper, density-stratified waters.
   The only exceptions to rather deeper water conditions prevailing during gypsum (and related clystone) deposition are exposure episodes following deposition of giant gypsum intergrowths and during the alabastrization phases. Particular gypsum units are common throughout the quarry, although some distinct lateral changes are observed. Amount of clay material in the facies of giant gypsum intergrowths increase toward the east and this increase is accompanied by change of massive facies to skeletal facies of giant gypsum intergrowths. Also the thickness of laminated gypsum units as well as the number and thickness of breccias in the upper part of gypsum sequence increase toward the east, whereas the frequency of amalgamates of supercones decrease toward the east. These changes observed in the quarry reflect the presence of a paleoslope
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    21. 1. 2008
Datum importu
    8. 8. 2012