The complex geodynamic history of the Paratethys periodically fostered the evolution of a
highly endemic biota with only limited exchange between the neighboring Mediterranean …

The Neogene Styrian Basin is the westernmost sub-basin of the Pannonian Basin System.
The last comprehensive studies on the basin were published in the last millennium. This …

The Miocene Central Paratethys Sea covered wide areas of the Pannonian Basin System,
bordered by the mountain chains of the Alps, Carpathians and Dinarides. The epicontinental …

A new and precisely defined chronometric subdivision of the Badenian (Middle Miocene,
regional stage of Central Paratethys) is proposed. This uses global events, mainly …

Abstract The Alps and Western Carpathians constitute that part of the Alpine-Mediterranean
orogenic belt which advances furthest to the north into Central Europe. They were formed by …

Depositional sequences originating in semi-enclosed basins with endemic biota, partly or
completely isolated from the open ocean, frequently do not allow biostratigraphic …

We present a revision of geological and palaeontological data of the Vienna Basin. The
deposits comprise Miocene terrestrial, lacustrine and marine sediments, corresponding to …

For the first time, a concise lithostratigraphic scheme for the lower and middle Miocene
(Ottnangian–Badenian) of the northern and central Vienna Basin is proposed, which is …

Location limitation of logged wells restricts the porosity estimation across the whole reservoir
target, whereas seismic data are always collected to cover larger areas. In this paper …

Abstract The Vienna Basin (VB) originated during the early Miocene and represents one of
the largest onshore oil and gas field in Europe. The VB is composed of several horst and …