… The Pol ish part of the Cen tral Eu ro pean Variscan fore land in cludes sev … the south ern
mar gin of the Old Red Con ti nent. Dur ing the De vo nian to Namurian A, ar eas lo cated to the …

… elucidate the complex stratigraphy of the Carboniferous succession of the southwestern
Poland… interpretation of the stratigraphy and partly clarify timing of Carboniferous deposition and …

… to the SW border of the TESZ in Poland. This border is defined by the Dolsk Fault Zone (DFZ)
and the … developed as a result of the Variscan collision between Laurussia and Gondwana. …

… The stratigraphic succession records a steady sea-… the Devonian till the Early Carboniferous.
Particularly, no remarkable regression is noticeable in the Famennian, in contrast to the …

… USCB, within deep Tertiary grabens, down to 1,000 m deep, we can postulate the occurence
in the top part of the Carboniferous formation of pore waters squeezed out from Tertiary …

… in terms of sequence stratigraphy and chronostratigraphy of the Carboniferous deposits in
the LB. The aim of this study is also to reconstruct the environments and subenvironments, as …

… Tectonic setting of the Carboniferous basin of Poland at the northern flank of the Variscan
orogen. Variscan belt: MGCH Mid-German Crystalline high, MO Moldanubian zone, MS …

… The aim of this paper is to provide the geodynamic evolution and position of the major tectonic
elements of the area within the … Sweden, the Baltic Sea, and Poland; probably beneath the …

… , as well as on the older crystalline … the Carboniferous succession and the base of this
younger complex declines from 200 m below sea level in the east to about 1000 m in the SW of the …

… The base of the Carboniferous System is defined at the first appearance of the conodont
Siphonodella sulcata within the evolutionary lineage from Siphonodella praesulcata to Siphono-…