Number of the records: 1  

Thermal and tectonic history of the Barrandian Lower Paleozoic, Czech Republic: is there a fission-track evidence for Carboniferous-Permian overburden and pre-Westphalian alpinotype thrusting? (Critical comments on the paper by Ulrich Mann and Günter A. Wagner)

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    SYSNO ASEP0103943
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve SCOPUS
    TitleThermal and tectonic history of the Barrandian Lower Paleozoic, Czech Republic: is there a fission-track evidence for Carboniferous-Permian overburden and pre-Westphalian alpinotype thrusting? (Critical comments on the paper by Ulrich Mann and Günter A. Wagner)
    TitleTeplotní a tektonická historie barrandienského spodního paleozoika, Česká republika: existuje důkaz, podaný metodou štěpných stop, karbonsko-permského překrytí a předvestfálského alpinotypního příkrovu? (Kritické připomínky k článku Ulricha Manna a Günthera A. Wagnera)
    Author(s) Filip, Jiří (GLU-S) RID, SAI
    Suchý, V. (CZ)
    Source TitleBulletin of Geosciences. - : Česká geografická společnost - ISSN 1214-1119
    Roč. 79, č. 2 (2004), s. 107-112
    Number of pages6 s.
    Languageeng - English
    CountryCZ - Czech Republic
    Keywordsapatite fission-track analysis ; Barrandian ; Variscan Orogeny
    Subject RIVDB - Geology ; Mineralogy
    R&D ProjectsIAA3012703 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    EID SCOPUS4644280247
    AnnotationClose scrutiny of apatite fission-track data from Barrandian Lower Paleozoic rocks shows that previous interpretations involving a late Carboniferous to Permian heatingh stage and the extensive development of pre-Westphalian thrust tectonics are largely speculative. An alternative time-temperature path for the Barrandian sequence based on firmly established constraints and improved version of the AFTSolve annealing kinetic model by Ketcham at al. (2000) is presented as evidence of a simple late Devonian to early Carboniferous Variscan peak heating, followed by a gradual mesozoic to Tertiary cooling.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Tel.: 226 800 273
    Year of Publishing2005
Number of the records: 1  

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