Allowing for the palinspastic restoration of Tertiary strike-slip and extensional faulting it is
concluded that the Pannonian Basin is superposed on a Middle Cretaceous thrust and fold …

Mesozoic igneous rocks occur in various tectonic units of the Intra-Carpathian Area of
Eastern Europe. These rocks were situated several hundred km apart from one another …

Abstract The South Alpine–Dinaridic realm was affected by igneous activity in the Middle
Triassic; the marine carbonate platforms and the adjacent basins contain highly variable …

Abstract The Upper Eocene sequence of the Buda Hills consists of fluvial and shallow
marine conglomerates, sandstones, bioclastic shallow-water limestone, marlstone and …

The Vöröstó (= Red Lake) Formation, located in the Southern Bakony Mountains and the
Balaton Highlands (Hungary), is a red, clayey continental assemblage containing hard, up to …

In the Transdanubian Central Range, Middle Triassic formations are known on the surface in
the Balaton Highland, in the southern rim of the Veszprém Plateau, in the Eastern Bakony …

In the Pannonian Basin three Paleogene igneous regions can be outlined, namely the Zala
Basin Shear Zone, the Velence Mts and the Recsk Region. These igneous regions are …

In the Transdanubian Range, Pannonian Basin, Hungary, karstic sinkholes on a planation
surface of Triassic carbonates are filled by grey clayey–silty kaolin deposits. The …

Large, irregular volumes of altered, friable Triassic dolomite with poorly recognizable
depositional fabrics crop out in the Buda Mountains, Hungary. These rock volumes are …

The provenance of igneous clasts and arenitic sediment enclosed within the Bakony
Molasse was studied using geochemical and geochronological methods. The majority of …