Podrobnosti záznamu

Název
    The 87Rb-86Sr isotope geochemistry of the blueschist and greenschist metavolcanics of the Rýchory Mts. crystalline complex, West Sudetes, Bohemian Massif
Údaj o odpovědnosti
    Jiří Bendl, František Patočka, Edvín Pivec
Autor
    Bendl, Jiří
    Patočka, František
    Pivec, Edvín
Jazyk
    anglicky
Zdrojový dokument - seriál
    Geologia sudetica
Svazek/č.
    Vol. 30
Strany
    p. 3-20
Rok
    1997
Poznámky
    4 obr., 2 fot., 1 tab., 4 s.bibl.
    Zkr. název ser.: Geol. sudetica.
Předmětová skupina
    břidlice modrá
    břidlice zelená
    datování Rb/Sr
    geochemie izotopická
    kambrium
    krkonošsko-jizerské krystalinikum
    metavulkanity
    ordovik
    petrogeneze
    protolit
Geografické jméno
    ČR-Čechy
    Svoboda nad Úpou (Trutnov)
    Žacléř (Trutnov)
Klíčové slovo
    87Rb-86Sr
    Blueschist
    Bohemian
    Complex
    Crystalline
    Geochemistry
    Greenschist
    Isotope
    Massif
    Metavolcanics
    Mts
    Rýchory
    Sudetes
    West
Abstrakt (anglicky)
   The blueschists and greenschists of the Radčice group (the Rýchory Mts complex, West Sudetes) were analysed for Rb-Sr isotopes. The 87Sr/86Sr values of the metabasites, recalculated to Early Cambrian-Early Ordovician ages presumed for their magmatic origin. are mostly scattered between values of mantle-derived igneous rocks and Early Paleozoic oceanic waters. Either an introduction of seawater Sr into protolith or secondary alteration of Rb-Sr system during regional metamorphism can be a reason of this feature. Two extremely high Sr isotope values possibly indicate an input of radiogenic Sr leached from rocks of continental crust by postmagmatic hydrothermal alteratios and/or metamorphic fluids. Due to the scatter of the measured values in the Rb-Sr diagram it is impossible to derive an isochron and initial Sr isotope ratio valid for the whole sample set of the metabasites. However, two blueschists only weakly altered, are giving value 0.7039 as initial 87Sr/86Sr ratio.
   Thus a mantle-derived origin of the primary rocks can be presumed. The "isochron" defined by these samples in the Rb-Sr plot may be an indication of the Late Proterozoic to Early Ordovician magmatic age of the metabasite protolith. The Early Ordovician age may be accepted provided that the Radčice Group metabasite protolith took origin during hypothetic early-stage seafloor spreading, following on the intracontinental rifting dated to the same period by bimodal volcanism of the East Krkonoše Mts. This event would be set into the concept of Early Paleozoic rifting and opening of oceanic basins along the northern periphery of Gondwana
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    20. 2. 2008
Datum importu
    8. 8. 2012