Podrobnosti záznamu

Název
    Early Carboniferous Rb-Sr mica - whole-rock ages of phases of medium- and low-pressure metamorphism in the saxothuringian zone, western Bohemia
Údaj o odpovědnosti
    D.R. Bowes, C. M. Farrow, A. M. Hopgood, Emil Jelínek, Jan Košler, Graeme Rogers
Autor
    Bowes, D. R.
    Farrow, C. M.
    Hopgood, A. M.
    Jelínek, Emil, 1943-
    Košler, Jan, 1965-
    Rogers, Graeme
Jazyk
    anglicky
Zdrojový dokument - seriál
    Neues Jahrbuch für Mineralogie. Abhandlungen
Svazek/č.
    Vol. 175, no. 1
Strany
    p. 83-103
Rok
    1999
Poznámky
    2 obr., 1 fot., 3 tab., 4 s.bibl.
    Zkr. název ser.: Neu. Jb. Mineral., Abh.
Předmětová skupina
    břidlice chloritická
    chlority
    datování Rb/Sr
    deformace
    krušnohorské krystalinikum
    metamorfóza nízkostupňová
    slídy
    vrásnění variské
Geografické jméno
    ČR-Čechy
    Kraslice (Sokolov)
    Rotava (Sokolov)
Klíčové slovo
    Ages
    Bohemia
    Carboniferous
    Early
    Low-pressure
    Medium-
    Metamorphism
    Mica
    Phases
    Rb-Sr
    Saxothuringian
    Western
    Whole-rock
    Zone
Abstrakt (anglicky)
   A Rb-Sr white mica- whole-rock age of 327 6 Ma for a muscovite-paragonite, chlorite schist in the eastern Fichtelgebirge, near Kraslice, is recorded and interpreted as the time of the D2-S2 event at the peak of Barrovian-type dynamothermal metamorphism. A corresponding age of 327 5 Ma, obtained using the same isotopic system in another mica schist from the same district, is also recorded for a muscovite porphyroblast - whole-rock. The age is interpreted as the time of cooling through the closure temperature of muscovite following the overgrowth of randomly-disposed porphyroblasts and of paragonite-out reactions resulting from a low-pressure metamorphic overprint that had reset the Rb-Sr isotopic systems relatively late in the deformation sequence. With formation of three sets of thrusts that were major contributors to the tectonic stacking of the disparate crystalline units in the western part of the Bohemian Massif and of a number of sets of fold being between the two ca.
   330-325 Ma metamorphic events in the deformational sequence, the timing of the Hercynian orogenic episode in the southern Fichtelgebirge tectonic domain is deduced to have staddled the Viseán-Namurian boundary. The new data together with the ca. 320 Ma age of emplacement of the earliest of the granites in the Fichtelgebirge indicate a relatively short time span for this late Early Carboniferous episode during ehich (1) compressional tectonism, expressed by the development of intrafolial folds and schistosity during medium-pressure dynamothermal metamorphism, and then by sets of thrusts and upright folds, was followed by (2) a low-pressure metamorphic overprint and then by (3) further weak compressional ( transpressional) tectonism with the deformation of upright folds and then a set of thrusts
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    14. 2. 2008
Datum importu
    8. 8. 2012