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
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SYSNO ASEP 0348408 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název 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 Tvůrce(i) Hrubcová, Pavla (GFU-E) ORCID, RID
Środa, P. (PL)
Grad, M. (PL)
Geissler, W.H. (DE)
Guterch, A. (PL)
Vozár, J. (SK)
Hegedüs, E. (HU)Zdroj.dok. Geophysical Journal International - ISSN 0956-540X
Roč. 183, č. 2 (2010), s. 611-633Poč.str. 23 s. Jazyk dok. eng - angličtina Země vyd. GB - Velká Británie Klíč. slova controlled source seismology ; body waves ; continental margins: convergent ; crustal structure ; Europe Vědní obor RIV DC - Seismologie, vulkanologie a struktura Země CEP GAP210/10/2063 GA ČR - Grantová agentura ČR CEZ AV0Z30120515 - GFU-E (2005-2011) UT WOS 000283172100009 DOI 10.1111/j.1365-246X.2010.04766.x Anotace 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. Pracoviště Geofyzikální ústav Kontakt Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Rok sběru 2011
Počet záznamů: 1