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A short introduction to the geology, structural evolution, geophysical fields and geokinematics of the area studied by the CERGOP-2 countries and work package subgroups

Glazek J., Liszkowski J., Śledziński J., Vyskocil P.

Reports on Geodesy

2006

z. 4/79

19-53

Looking at the geological map (Fig.l) and the geotectonic division of Europe (inset scheme on Fig.l) we can see, that the area investigated by the 7 groups for regional investigation (WP 10.1 to WP 10.7) of the CERGOP - 2 work package WP 10 "Geodynamics of Central Europe" (see tab. 1 for subjects and chairs) belongs almost exclusively to the Alpine Europe, called also Neo-Europe, a sector of the Alpine-Himalayan erogenic belt. More exactly this includes mountain chains from the Eastern Alps through Carpathians to Balkanides on the northern and north-eastern side of the major Alpine suture zone known in the Eastern Alps as Gailtal Line through substrate of Neogene Pannonian Basin to the Vardar Zone and the Southern Alps through Dinarides to the Hellenides on the southern and south-western side of these suture zone (Ager 1980, Peive et al. 1982 and Fig. 2). The forefield of the Eastern Alps-Carpathians-Balkans Alpine fold-and-thrust belt is very heterogenous and comprise tectonic units of Variscan (=Hercynian, e.g. Bohemian Massif of Czech Republic including the neighbouring strips of Austria, Germany and Poland), Caledonian (?, suggested within the Transeuropean Suture Zone - TESZ - of northern Germany and Poland, by Stille 1950, Znosko 1986 and questioned by Glazek 1995, Malinowski et al. 2005, Guterch & Grad 2006; cf. Fig. 3), and Ancient East European Craton - EEC (Ukrainian-Moldavian sector of the East-European Platform). To the SE the TESZ is covered by Alpine structures of the East Carpathians and again emerges in Dobrogea close to Black Sea (Fig. 2). There TESZ divide the EEC from the late Precambrian Moesian Platform (in Romania and Bulgaria) squeezed in between Balkanides (=Stara Planina) and southern Carpathians (Peive et. al. 1981,1982). These structures were described in details in a series of monographs published in Reports on Geodesy by the Chief Editor J.Sledzinski as results of the CERGOP-1 Study Group CSG 8 "Geotectonic analysis of the region of Central Europe".