Results 1 to 10 of about 190,285 (154)

Mélange, Flysch and Cliffs in the Pieniny Klippen Belt (Poland): An Overview

open access: yesMinerals (Basel, Switzerland), 2022
The Pieniny Klippen Belt (PKB) is located in the suture zone between the Central and Outer (Flysch) Carpathians. Its structure is an effect of prolonged processes of the Cretaceous–Miocene folding, thrusting and uplifting. In this zone, tectonic components of different ages and features, including strike-slip-bounded tectonic blocks, thrust units, as ...
Kamil Cichostępski, Jerzy Dec
exaly   +4 more sources

Deep structure of the Pieniny Klippen Belt in Poland

open access: yesSwiss Journal of Geosciences, 2019
An interpretation of the deep structure of the Pieniny Klippen Belt in Poland is presented, utilizing a high-resolution deep seismic reflection survey. The studied profiles reach a depth of around 23 km. The seismic lines depict the structure and mutual relationships between the main domains analyzed—the Central Carpathians (CC), the Pieniny Klippen ...
Monika Kasperska, Kamil Cichostępski
exaly   +4 more sources

Biostratigraphic significance of calcareous dinocysts in the Tithonian of the Pieniny Klippen Belt (southern Poland) [PDF]

open access: yesPeerJ
Biostratigraphic studies of pelagic Tithonian limestones in the Western Tethys are important for regional palaeoenvironmental reconstructions, particularly for determining the onset of the accumulation of Maiolica-type sediments which dominated Early ...
Agnieszka Ciurej   +3 more
doaj   +6 more sources

Shallow Seismic Refraction Tomography Images from the Pieniny Klippen Belt (Southern Poland)

open access: yesMinerals (Basel, Switzerland)
The Pieniny Klippen Belt (PKB) is located between the Central and the Outer (Flysch) Carpathians and forms a narrow zone with a complex structure, often described as a mélange. It is composed of numerous tectonic elements of different size including strike-slip-bounded tectonic blocks, thrust units, toe thrusts and olistostromes combined together and ...
Kamil Cichostępski, Jerzy Dec
exaly   +4 more sources

Late Cretaceous age of magmatism at Vršatec in the Pieniny Klippen Belt, Western Carpathians, Slovakia

open access: yesMineralogia
Volcanic rocks in the Pieniny Klippen Belt (PKB) of the Western Carpathians have been the focus of geologists for over a century (e.g. Uhlig, 1890; Małkowski, 1921). Miocene volcanism is most common in the PKB.
Bazarnik Jakub   +5 more
doaj   +4 more sources

Geodynamic Studies in the Pieniny Klippen Belt in 2004–2020 [PDF]

open access: yesArtificial Satellites, 2023
ABSTRACT The Pieniny Geodynamic Test Field is situated in the middle of the region between the Inner and Outer Carpathians. Geodynamic research conducted in the past in the Pieniny Klippen Belt (PKB) region were suggestive of neotectonic activity.
Dominika Staniszewska   +4 more
semanticscholar   +3 more sources

The Babín Klippen – a peculiar branch of the Orava sector of the Pieniny Klippen Belt (Slovakia)

open access: yesMineralia Slovaca
The Pieniny Klippen Belt (PKB) is a narrow, approx. 5 – 8 km wide zone at the boundary of the External and Internal Western Carpathians. The zone of the Babín Klippen, which is the main subject of this study, represents northerly situated branch of the ...
František Teťák   +2 more
doaj   +3 more sources

Linkage of the Manín and Klape units with the Pieniny Klippen Belt and Central Western Carpathians: balancing the ambiguity

open access: yesGeologica Carpathica, 2019
The paper deals with the structure and evolution of the Pieniny Klippen Belt in its classic area in western Slovakia. The so-called Peri-Klippen Zone provides a transition from the Pieniny Klippen Belt s.s.
Plašienka Dušan
doaj   +3 more sources

Crustal deformation from GNSS measurement and earthquake mechanism along Pieniny Klippen Belt, Southern Poland

open access: yesArabian Journal of Geosciences
AbstractThe dynamic geological features of the Pieniny Klippen Belt (PKB) in southern Poland are nowadays a focal point of researchers as it is recognised as an active zone of crustal discontinuity. In the present study, we employed long-term analysis of ground-based global navigation satellite system (GNSS) measurements (from 2004 to 2020) to probe ...
Kinga Wezka   +2 more
exaly   +3 more sources

Cadosinopsis rehakovii sp. nov., a new calcareous dinocyst from the Jurassic-Cretaceous transitional interval of the Western Tethys. [PDF]

open access: yesPLoS ONE, 2021
Variegated limestones, a transitional series between red, Upper Jurassic radiolarite and whitish, Lower Cretaceous Maiolica limestone in the Pieniny Klippen Belt deposits in the Polish part of the Western Carpathians, have yielded rich microfossil ...
Agnieszka Ciurej, Marta Bąk
doaj   +2 more sources

Home - About - Disclaimer - Privacy