At the end of the Eocene, the demise of the Tethys Ocean led to the formation of one of the
largest anoxic seas in the last 50 million years of Earth history. This long-lived anoxic water …

Global sea-level fall during the late Eocene-Oligocene icehouse, in conjunction with the
Alpine orogenesis, resulted in the epicontinental Paratethys Sea formed at the northern …

The early Alpine tectonic evolution of the Western Carpathian orogenic system is
differentiated into four main periods:(i) Middle‐Late Triassic rifting and spreading of the …

ABSTRACT The Western Carpathians in the territory of Moravia (the eastern part of the
Czech Republic) and northeastern (Lower) Austria represent the westernmost segment of …

Abstract The Western Carpathians are separated into an Outer and Inner Carpathians (both
comprising several nappe systems) by the extremely narrow and highly deformed Pieniny …

The Polish Outer Carpathians (POC) form part of the arcuate Carpathian mountain system,
that extends over more than 1300 km from the Danube valley in Austria to the Danube valley …

AAPG Datapages/Archives: Plate-tectonic Evolution and Paleogeography of the Circum-Carpathian
Region Datapages Datapages Home Associated Websites Archives Search and Discovery GIS …

This study presents first isoscape maps of strontium isotope signatures and their spatial
variation in Poland, based on~ 900 samples of rocks, sediments, surface water, and flora …

New balanced and restored cross-sections and a 2D kinematic model illustrate the present
geometry of the northeastern Outer Carpathians and quantify their orogenic evolution …

Abstract The Chornohora and Svydovets massifs represent the highest part of the Ukrainian
Carpathians (2061 m asl) and the north-eastmost mountain area in Europe, which was …