As a complex paleo-ocean located between the Tarim-North China and the
Sibumasu/Baoshan blocks, the Proto-Tethys Ocean was opened from the rifting of the …

Global plate motion models provide a spatial and temporal framework for geological data
and have been effective tools for exploring processes occurring at the earth's surface …

We present a map that correlates tectonic units between Alps and western Turkey
accompanied by a text providing access to literature data, explaining the concepts used for …

Abstract The Late Cretaceous was a time of tremendous global change, as the final stages
of the Age of Dinosaurs were shaped by climate and sea level fluctuations and witness to …

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 …

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 …

ABSTRACT The Polish and Ukrainian Carpathian Foredeep, about 600 km (376 mi) long
and as much as 100 km (62 mi) wide, is part of the large sedimentary basin that stretches for …

The data about the Paleogene basin evolution, palaeogeography, and geodynamics of the
Western Carpathian and Northern Pannonian domains are summarized, re-evaluated …

Limestones designated the Štramberk-type are the most common carbonate exotic clasts
(exotics) embedded in the uppermost Jurassic–Miocene flysch deposits of the Polish Outer …

A complex interplay of palaeoclimatic, eustatic and tectonic processes led to fragmentation
and dissipation of the vast Tethys Ocean in Eocene–Oligocene times. The resulting …