Results 31 to 40 of about 190,285 (154)
Discussion of ‘Olistostromes of the Pieniny Klippen Belt, Northern Carpathians’
J. Golonka, M. Krobicki, A. Waśkowska, M. Cieszkowski & A. Ślączkareply: We welcome the comments by our Slovakian colleagues and their critique of our results, particularly as we have discussed and published papers together several times about our ideas, sometimes, more or less, disputable (Aubrechtet al.2003, 2006; Krobickiet al.2003; Krobicki ...
J. Golonka +5 more
openaire +3 more sources
Gravity measurements in the Pieniny Klippen Belt (Western Slovakia) [PDF]
1 Slovak Academy of Sciences, Geophysical Insitute; Dubravska cesta 9, 845 04 Bratislava, Slovakia; e-mail: geofjabu@savba.sk 2 GEOFOS, s.r.o.; Veľký diel 3323, 010 08 Žilina, Slovakia 3 Comenius University, Faculty of Natural Sciences, Department of Applied and Environmental Geophysics; Mlynska dolina, 842 15 Bratislava 4, Slovakia 4 Comenius ...
Jana Bucová +3 more
openaire +1 more source
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
Olistostromes of the Pieniny Klippen Belt, Northern Carpathians
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
The Czertezik Succession of the Pieniny Klippen Belt in Poland is assigned herein to its type area of occurrence – the main Pieniny Range, between Zamkowa Góra and Czertezik mounts.
A. Wierzbowski +3 more
semanticscholar +1 more source
Deep contact of the Bohemian Massif and Western Carpathians as seen from density modeling
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
: The Pieniny Klippen Belt of the Western Carpathians is built up by Jurassic to Eocene Oravic units, with the Šariš, Subpieniny, and Pieniny Unit on the top.
Marína Molčan Matejová, P. Gedl
semanticscholar +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]
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 +3 more
core +2 more sources
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
The Jurassic to Palaeogene strata in the northern boundary fault zone in deep borehole PD-9 at Szczawnica, Pieniny Klippen Belt, West Carpathians, Poland: biostratigraphy and tectonic implications [PDF]
The Jurassic through Palaeogene stratigraphy and tectonic structure of the PD-9 borehole at Szczawnica, Pieniny Klippen Belt, West Carpathians, Poland, is revised.
Gedl, Przemysław +1 more
core +1 more source

