Počet záznamů: 1

From the Variscan to the Alpine Orogeny: crustal structure of the Bohemian Massif and the Western Carpathians in the light of the SUDETES 2003 seismic data

  1. 1.
    0348408 - GFU-E 2011 RIV GB eng J - Článek v odborném periodiku
    Hrubcová, Pavla - Środa, P. - Grad, M. - Geissler, W.H. - Guterch, A. - Vozár, J. - Hegedüs, E.
    From the Variscan to the Alpine Orogeny: crustal structure of the Bohemian Massif and the Western Carpathians in the light of the SUDETES 2003 seismic data.
    Geophysical Journal International. Roč. 183, č. 2 (2010), s. 611-633 ISSN 0956-540X
    Grant CEP: GA ČR GAP210/10/2063
    Výzkumný záměr: CEZ:AV0Z30120515
    Klíčová slova: controlled source seismology * body waves * continental margins: convergent * crustal structure * Europe
    Kód oboru RIV: DC - Seismologie, vulkanologie a struktura Země
    Impakt faktor: 2.411, rok: 2010

    The Variscan orogeny is the major Middle to Late Palaeozoic tectonometamorphic event in central Europe, and the Bohemian Massif is the largest exposure of rocks deformed during this orogeny. The Bohemian Massif consists of the Saxothuringian, Barrandian and Moldanubian units. Adjacent to this massif in the southeast, the Western Carpathians form an arc-shaped mountain range related to the Alpine orogeny during the Cretaceous to Tertiary. The complex crustal-scale geological structure of the Variscan Bohemian Massif and the Western Carpathians, and especially their contact, were analysed in this study employing the data of the SUDETES 2003 international seismic refraction experiment.
    Trvalý link: http://hdl.handle.net/11104/0188955