[PDF][PDF] Jurassic syn-rift and Cretaceous syn-orogenic, coarse-grained deposits related to opening and closure of the Vahic (South Penninic) Ocean in the Western …

D Plasienka - Geological Quarterly, 2012 - bibliotekanauki.pl
Although no undoubted oceanic crustal rock complexes of Penninic affinity participate in the
present surface structure of the Western Carpathians, indirect lines of evidence suggest …

Neogene palaeogeography and basin evolution of the Western Carpathians, Northern Pannonian domain and adjoining areas

M Kováč, E Márton, N Oszczypko, R Vojtko… - Global and Planetary …, 2017 - Elsevier
The data on the Neogene geodynamics, palaeogeography, and basin evolution of the
Western Carpathians, Northern Pannonian domain and adjoining areas (ALCAPA Mega …

Evolution of Late Cretaceous-Palaeogene synorogenic basins in the Pieniny Klippen Belt and adjacent zones (Western Carpathians, Slovakia): tectonic controls over …

D Plašienka, J Sotak - Annales Societatis Geologorum Poloniae, 2015 - infona.pl
The Pieniny Klippen Belt and neighbouring zones of the Western Carpathians represent an
ancient accretionary wedge that developed during the meso-Alpidic (Coniacian–Eocene) …

Palaeogene and Neogene

MW Rasser, M Harzhauser, OY Anistratenko… - 2008 - pubs.geoscienceworld.org
Over the last 65 Ma, our world assumed its modern shape. This timespan is divided into the
Palaeogene Period, lasting from 65 to 23 Ma and the Neogene, which extends up to the …

Sedimentology and hydrocarbon habitat of the submarine-fan deposits of the Central Carpathian Paleogene Basin (NE Slovakia)

J Soták, M Pereszlenyi, R Marschalko, J Milicka… - Marine and Petroleum …, 2001 - Elsevier
The Central Carpathian Paleogene Basin accommodates a subsiding area of the destructive
plate-margin. The basin history comprises marginal faulting and alluvial fan accumulation …

Variable structural styles and tectonic evolution of an ancient backstop boundary: the Pieniny Klippen Belt of the Western Carpathians

D Plašienka, J Bučová, V Šimonová - International Journal of Earth …, 2020 - Springer
Abstract The Pieniny Klippen Belt (PKB) and adjoining zones form a narrow, but lengthy belt
that separates the Cretaceous nappe stack of the Central (Austroalpine) and the Cenozoic …

[PDF][PDF] Late Eocene to Quaternary deformation and stress field evolution of the Orava region (Western Carpathians)

I Pešková, R Vojtko, D Starek, Ľ Sliva - Acta Geologica Polonica, 2009 - geo.sav.sk
The northern part of the Western Carpathians suffered polyphase deformation at the
boundary between their Central and Outer parts. Palaeostress analysis in the Orava region …

[PDF][PDF] Miocene basin opening in relation to the north-eastward tectonic extrusion of the ALCAPA Mega-Unit

M Kováč, E Márton, T Klučiar… - Geologica …, 2018 - geologicacarpathica.com
The opening and evolution of the Western Carpathians Miocene basins was closely related
to the northeastward tectonic extrusion of the ALCAPA Mega-Unit lithosphere caused by the …

[PDF][PDF] Reconstruction of Cenozoic paleostress fields and revised tectonic history in the northern part of the Central Western Carpathians (the Spisská Magura and …

R Vojtko, E Tokárováá, L Sliva… - Geologica …, 2010 - geologicacarpathica.com
This study investigates the chronology of paleostress evolution and faulting in the northern
part of the Central Western Carpathians (Spišská Magura and Východné Tatry Mts) …

[PDF][PDF] Early stages of structural evolution of the Carpathian Klippen Belt (Slovakian Pieniny sector)

D PLAšIENKA - Mineralia Slovaca, 2012 - geology.sk
Abstract The Pieniny Klippen Belt (PKB) is a distinctive, suture-like tectonic zone that
separates the External Carpathian Tertiary accretionary wedge (Flysch Belt) and the …