Lithosphere structure of the NE Bohemian Massif (Sudetes) — A teleseismic receiver function study

0381573 - GFÚ 2013 RIV NL eng J - Článek v odborném periodiku
Geissler, W.H. - Kämpf, H. - Skácelová, Z. - Plomerová, Jaroslava - Babuška, Vladislav - Kind, R.
Lithosphere structure of the NE Bohemian Massif (Sudetes) — A teleseismic receiver function study.
Tectonophysics. 564-565, Sep 5 (2012), s. 12-37. ISSN 0040-1951. E-ISSN 1879-3266
Grant CEP: GA ČR GA205/07/1088; GA ČR GAP210/12/2381; GA MŠMT LM2010008
Výzkumný záměr: CEZ:AV0Z30120515
Klíčová slova: lithospheric structure * Moho discontinuity * lithosphere-asthenosphere boundary * Permo-Carboniferous volcanism * Central Europe
Kód oboru RIV: DC - Seismologie, vulkanologie a struktura Země
Impakt faktor: 2.684, rok: 2012

In 2004 and 2005 a passive seismic experiment was carried out in the northern and northeastern part of the Bohemian Massif (Sudetes) to study the lithospheric structure. We present results from Ps and Sp receiver function analyses. With one exception, Moho depth at stations in the northwestern part of the study area varies between 28 and 32 km. Thicker crust up to 35 km was mapped toward the south (Moldanubian unit) and toward the east (Moravo–Silesian and Brunovistulian units) confirming results from previous active seismic measurements. There exists a relatively sharp step in Moho depth between units of the central Sudetes.
Trvalý link: http://hdl.handle.net/11104/0212010