The structure of the Western Outer Carpathians on Austrian, Slovak, Czech and Polish
territory is an effect of prolonged processes of Cretaceous to Miocene folding, nappe …

Beaver (Castor sp.) can change the riverine environment through dam-building and other
activities. The European beaver (Castor fiber) was extirpated in Poland by the nineteenth …

Crystalline exotic boulders within the sedimentary sequences of the Outer Carpathians likely
represent Proto-Carpathian basement, which was exposed and eroded during the Mesozoic …

Mainly pelagic/hemipelagic deposits of the Vezhany Nappe (Paleocene-Lowermost
Oligocene Metova Formation with a high content of planktonic foraminifera) and typical …

Petrographic examination, heavy mineral analysis and detrital zircon U-Pb dating were
performed on the Eocene siliciclastic rocks in the Rača Unit of the Outer Western …

Based on the interpretation of 2D seismic profiles integrated with surface geological
investigations, a mechanism responsible for the formation of a large scale normal fault zone …

The biostratigraphy of the Outer Carpathians is based mainly on the ranges of agglutinated
foraminifera. Species acmes provide the opportunity to enhance and support the existing …

The Magura Nappe in the Polish sector of the Outer Carpathians consists of four tectonic
subunits characterized by differing development of facies. From the south to the north, they …

The present authors investigated the Paleogene deposits of the internal zone of the Magura
Basin known as the Krynica Subunit or Krynica zone in Poland. These deposits crop out in …

The sedimentation of Hieroglyphic beds of the Silesian Nappe took place between the
Lower and Middle Eocene and Upper Eocene within the Carpathian Silesian Basin. These …