%0 Journal Article
%T Continuation of the Pohorel¨˘ line in pre-Cenozoic basement of the Central Slovakia Volcanic Field (Western Carpathians)
%A Jozef H¨®k
%A Rastislav Vojtko
%J Acta Geologica Slovaca
%D 2011
%I Comenius University in Bratislava
%X The Pohorel¨˘ line (PL) is an important tectonic element dividing the major pre-Cenozoic lithotectonic units of the Northern and Southern Veporicum. Moreover, the PL separates occurrences of the Gemericum, Meliaticum, and Silicicum on its S¨CSE side against the Fatricum and Hronicum on NW side. Continuation of the PL towards the SW was unknown because the pre-Cenozoic basement of the Veporic Unit is covered with Cenozoic (Neogene) volcanics and volcanosedimentary rocks. Reinterpretations of the deep boreholes data reveal a outhwest continuation of the PL to the Po ana, Javorie, and  tiavnica stratovolcanic complexes basement and then further towards the SSW.
%K Pohorel¨˘ line
%K Pre-Cenozoic basement
%K Veporicum
%K neovolcanite
%K Western Carpathians
%U http://www.geopaleo.fns.uniba.sk/ageos/archive/2011_01/hok_vojtko_2011.pdf