Results 21 to 30 of about 896 (145)

Transcarpathian Depression: Study of Low-Velocity Zones in the Earth’s Crust Based on the Seismic Regional Profiles Data

open access: yesГеофизический журнал, 2023
Transcarpathian depression (TD) is located in the junction zone of the eastern margin of ALCAPA terrain and the northern part of Tisza-Dacia one, buried under thick Neogene molasses. The Earth’s crust structure of the TD is not clearly understood. The
A. Murovskay   +4 more
doaj   +1 more source

Geological structure and evolution of the Pieniny Klippen Belt to the east of the Dunajec River : a new approach (Western Outer Carpathians, Poland) [PDF]

open access: yes, 2014
The area studied, known as the Małe (Little) Pieniny Mts., belongs to the Pieniny Klippen Belt (PKB), a suture zone that separates the Central Carpathians from the Outer Carpathian accretionary wedge. Along its northern boundary the PKB is separated from
Oszczypko, Nestor   +1 more
core   +1 more source

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

open access: yesMinerals, 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 ...
Jan Golonka   +8 more
openaire   +1 more source

Trace element geochemistry of the Early to Late Cretaceous deposits of the Grajcarek thrust-sheets : a palaeoenvironmental approach (Małe Pieniny Mts., Pieniny Klippen Belt, Poland) [PDF]

open access: yes, 2012
The chemical composition of the Cretaceous deposits of the Grajcarek thrust-sheets (Pieniny Klippen Belt, Poland) has been investigated to provide information on palaeoenvironment and provenance of pelagic and turbiditic particles.
Oszczypko, Nestor   +1 more
core   +1 more source

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   +1 more source

Early Cretaceous intra-plate volcanism in the Pieniny Klippen Belt : a case study of the Velykyi Kamenets'/Vilkhivchyk (Ukraine) and Biała Woda (Poland) sections [PDF]

open access: yes, 2012
The geological position and geochemistry of the basaltic sill and tuffs occurring within the Berriasian-?Albian pelagic limestones of the Czorsztyn Succession are described.
Krobicki, Michał   +2 more
core   +1 more source

Depth structure of the Transcarpathian Depression (Ukrainian part) according to density modeling data

open access: yesГеофизический журнал, 2023
The presented research is devoted to the construction and calculations of the density model along the regional CMRV-DSS profile RP-17 (Chop–Velykyy Bychkiv), running along the Transcarpathian depression.
I. Makarenko   +6 more
doaj   +1 more source

Cretaceous (Aptian/Albian-?Cenomanian) age of "black flysch" and adjacent deposits of the Grajcarek thrust-sheets in the Małe Pieniny Mts. (Pieniny Klippen Belt, Polish Outer Carpathians) [PDF]

open access: yes, 2012
Several sections record the relation between the "black flysch" and Upper Cretaceous red shales in the Grajcarek thrust-sheets. In all the sections studied the "black flysch" appears in the core of imbricated folds or thrust-sheets, whereas the limbs are
Malata, Ewa   +2 more
core   +1 more source

Olistostromes of the Pieniny Klippen Belt, Northern Carpathians

open access: yesGeological Magazine, 2014
AbstractThe olistostromes form two belts within the Pieniny Klippen Belt (PKB) in the Northern Carpathians. They mark an early stage of the development of the accretionary prism. The first belt was formed during Late Cretaceous time as a result of subduction of the southern part of the Alpine Tethys.
Golonka, Jan   +4 more
openaire   +2 more sources

Deep contact of the Bohemian Massif and Western Carpathians as seen from density modeling

open access: yesGeologica Carpathica, 2018
Density modelling was carried out along five profiles oriented across the expected deep contact between the Bohemian Massif and the Internal Western Carpathians in western Slovakia.
Šamajová Lenka   +3 more
doaj   +1 more source

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