Podrobnosti záznamu

Název
    Timing of Palaeozoic magmatism in the Maggia and Sambucco nappes and paleogeographic implications (Central Lepontine Alps)
Autor
    Bussien, Denise
    Bussy, Francois
    Magna, Tomáš
    Masson, Henri
Jazyk
    anglicky
Typ dokumentu
    článek v periodiku
Zdrojový dokument - seriál
    Swiss Journal of Geosciences
Svazek/č.
    Roč. 104, č. 1
Strany
    29
Rok
    2011
Výraz tezauru
    LA-ICPMS,U-Pb dating,zircon,granite,Variscan,Penninic,Swiss Alps
Klíčové slovo
    Alps
    Central
    Implications
    Lepontine
    Maggia
    Magmatism
    Nappes
    Palaeozoic
    Paleogeographic
    Sambucco
    Timing
Abstrakt (anglicky)
   Magmatic rocks from the pre-Mesozoic basements of the Sambuco and Maggia nappes have been dated by U-Pb zircon ages with the LA-ICPMS technique. Several magmatic events have been identified in the Sambuco nappe and the Cocco granodiorite and Rüscada leucogranite yielded ages of ca. 300-310 Ma; they are significantly older than former age determinations. The age coincidence strongly suggests paleogeographic proximity of the Sambuco and Maggia nappes in Late Carboniferous times. These two nappes have been interpreted as belonging to distinct Mesozoic paleogeographic domains: 'European' for Sambuco and 'Brianconnais' for Maggia, separated by the 'Valais' oceanic basin. In this case, the similarity of the Matorello and Cocco intrusions would demonstrate the absence of any significant transcurrent movement between these two continental domains. Alternatively, according to a more traditional view, Sambuco and Maggia might belong to a single large Alpine tectonic unit.
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (RIV)
Zdrojový formát
    R
Datum importu
    15. 10. 2014