Podrobnosti záznamu

Název
    Distribution and Origin of Reduction Spheroid in the Upper Paleozoic Sequences, Czech Republic
Údaj o odpovědnosti
    Vladimír Skoček
Autor
    Skoček, Vladimír, 1934-
Jazyk
    anglicky
Zdrojový dokument - seriál
    Věstník Českého geologického ústavu (Bulletin of the Czech Geological Survey)
Svazek/č.
    Vol. 74, no. 2
Strany
    p. 119-126
Rok
    1999
Poznámky
    3 obr., 6 fot., 1 tab., 28 bibl.
    České resumé
    Zkr. název ser.: Věst. Čes. geol. Úst. (Bull. Czech geol. Surv.)
Předmětová skupina
    diageneze
    Eh hodnota
    karbon-svrchní
    perm-spodní
    pH
    red beds
    sferule
    středočeské svrchní paleozoikum
    sudetské svrchní paleozoikum
    svrchní paleozoikum brázd
Geografické jméno
    Česká republika
Klíčové slovo
    Czech
    Distribution
    Origin
    Paleozoic
    Reduction
    Republic
    Sequences
    Spheroid
    Upper
Abstrakt (anglicky)
   Green spots or spheroids frequently occur in fluvio-lacustrine redbeds of the Stephanian C and Permian age whereas they are extremely rare in red sediments of the Stephanian A and totally lacking in red sediments of the Westphalian C and D. Cores are more common at certain levels whereas at other levels are totally absent due to processes leading to their erasing. In centres of spheroids, vanadium and uranium oxides, present as earthy porous matter or pigment of calcite crystals or concretions, often occur. The study of distribution has shown that spots originated in an early diagenetic stage, not deep below the sediment/atmosphere interface, probably within the zone of microbial activity. It is presumed that afluctuating moistening was one of the prerequisites of discrete sites origin which were centres of Fe3+ reduction. Such sites represented inhomogenieties with pH and Eh gradient compared to the hosting sediment.
   Organic matter and vanadium and uranium compounds played the decisive role in the process. The mobility of aforementioned elements was enhanced due to elevated temperature and fluctuating mineralization of pore solutions. The precipitation and following dissolution of V and U was accompanied by an irreversible Fe3+ removal. The uneven distribution of spheroids evidences their relation to diagenesis of porous sediments under specific and climatic circumstances. The classical explanation of spots as simple reduction features induced by fragments of plants, grains of mafic minerals or pyrite clusters is in contradiction to actual observations
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    19. 2. 2008
Datum importu
    8. 8. 2012