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Global continental and ocean basin reconstructions since 200 Ma
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 …
and have been effective tools for exploring processes occurring at the earth's surface …
Closure of the Proto-Tethys Ocean and Early Paleozoic amalgamation of microcontinental blocks in East Asia
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 …
Sibumasu/Baoshan blocks, the Proto-Tethys Ocean was opened from the rifting of the …
Tectonic units of the Alpine collision zone between Eastern Alps and western Turkey
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 …
accompanied by a text providing access to literature data, explaining the concepts used for …
Island life in the Cretaceous-faunal composition, biogeography, evolution, and extinction of land-living vertebrates on the Late Cretaceous European archipelago
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 marked …
of Dinosaurs were shaped by climate and sea level fluctuations and witness to marked …
Geology and hydrocarbon resources of the Outer Western Carpathians and their foreland, Czech Republic
FJ Picha, Z Strnk, O Krej - 2006 - archives.datapages.com
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 …
Czech Republic) and northeastern (Lower) Austria represent the westernmost segment of …
[PDF][PDF] A lost carbonate platform deciphered from clasts embedded in flysch: Štramberk-type limestones, Polish Outer Carpathians
M Hoffmann, B Kołodziej, J Kowal-Kasprzyk - 2021 - ruj.uj.edu.pl
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 …
(exotics) embedded in the uppermost Jurassic–Miocene flysch deposits of the Polish Outer …
The dire straits of Paratethys: gateways to the anoxic giant of Eurasia
DV Palcu, W Krijgsman - 2023 - pubs.geoscienceworld.org
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 …
and dissipation of the vast Tethys Ocean in Eocene–Oligocene times. The resulting …
Late Jurassic-Miocene evolution of the Outer Carpathian fold-and-thrust belt and its foredeep basin (Western Carpathians, Poland)
N Oszczypko - Geological Quarterly, 2006 - yadda.icm.edu.pl
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 …
that extends over more than 1300 km from the Danube valley in Austria to the Danube valley …
Paleogene palaeogeography and basin evolution of the Western Carpathians, Northern Pannonian domain and adjoining areas
The data about the Paleogene basin evolution, palaeogeography, and geodynamics of the
Western Carpathian and Northern Pannonian domains are summarized, re-evaluated …
Western Carpathian and Northern Pannonian domains are summarized, re-evaluated …
Transitional flow deposits on submarine lobe flank (Veřovice and Lhoty Fms, Albian–Cenomanian, Polish Outer Carpathians)
P Łapcik - Sedimentary Geology, 2023 - Elsevier
Abstract The Zagórnik-Rzyki studied section includes the upper part of the Veřovice Fm and
the lower part of the Lhoty Fm (Aptian–Albian), which are small fragments of the much …
the lower part of the Lhoty Fm (Aptian–Albian), which are small fragments of the much …