Podrobnosti záznamu

Název
    Post-collisional granite generation and HT-LP metamorphism by radiogenic heating: the Variscan South Bohemian Batholith
Údaj o odpovědnosti
    Axel Gerdes, Gerhard Wörner, Andreas Henk
Autor
    Gerdes, Axel
    Henk, Andreas
    Wörner, Gerhard
Jazyk
    anglicky
Zdrojový dokument - seriál
    Journal of the Geological society
Svazek/č.
    Vol. 157, no. 3
Strany
    p. 577-587
Rok
    2000
Poznámky
    6 obr., 2 tab., 3 s. bibl.
    il.
    Zkr. název ser.: J. Geol. Soc. (Bath)
Předmětová skupina
    granitoidy
    kolize desek
    litosféra
    metamorfóza vysokostupňová
    moldanubický pluton
    petrogeneze
    radioaktivita
    tepelný tok
    vlastnosti fyzikální
    vrásnění variské
    zkrácení kůry
Geografické jméno
    Česká republika
    Rakousko
Klíčové slovo
    Batholith
    Bohemian
    Generation
    Granite
    Heating
    HT-LP
    Metamorphism
    Post-collisional
    Radiogenic
    South
    Variscan
Abstrakt (anglicky)
   The Palaeozoic Variscan orogen of Europe is a well-documented example of a collision zone characterized by widespread late-orogenic high-temperature metamorphism and associated crustal magmatism. However, the heat source is still under debate. based on the Bohemian Massif in the internal zone of the Variscides as case study, we present geological, geochemical, petrological and geochronological data arguing against a substantial mantle involvement in metamorphism and magma genesis in the area of the South Bohemian Batholith. In order to provide an alternative explanation consistent with heat transfer mechanism, we apply a two-dimensional thermal-kinematic modelling approach. The model calculates the transient lithospheric temperature field during crustal thickening and subsequent thinning by erosion from material parameters and boundary conditions specific to the study area.
   Model results show that the increased contribution of radiogenic heat in the thickened crust can indeed cause a substantial temperature increase in the middle and lower crust. Model predictions are in good agreement with observations, e.g. the P-T-t evolution of the country rocks, the formation of syn-kinematic migmatites, the large volumes of peraluminous granites derived from dehydration melting of metasediments and the small volumes of lamprophyric melts from the mantle lithosphere. The results of this study emphasize the importance of radiogenic heat as the source for high-temperature metamorphism and granite petrogenesis in the Bohemian Massif and potentially in other areas of the Variscan Orogen
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    10. 11. 2006
Datum importu
    8. 8. 2012