Results 41 to 50 of about 1,578 (175)
Geologica Carpathica, 2022 : 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.
M. Molčan Matejová, P. Gedl
semanticscholar +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]
, 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
Geological 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
High (ultrahigh) pressure metamorphic terrane rocks as the source of the detrital garnets from the Middle Jurassic sands and sandstones of the Cracow Region (Cracow- Wieluń Upland, Poland) [PDF]
, 2012 The Middle Jurassic (Upper Bathonian/Lower Callovian) sands and sandstones of the Cracow–Wieluń Upland contain detrital garnets with high contents of the pyrope molecule (30–73 mol %).
Aubrecht, Roman +3 more
core +1 more source
Deep contact of the Bohemian Massif and Western Carpathians as seen from density modeling
Geologica 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
Геофизический 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
Minerals, 2021 The Grajcarek Unit of the Pieniny Klippen Belt (PKB), at the boundary between the Central (Inner) and Outer Carpathians, resulted from the convergence of the ALCAPA (the Alps–Carpathians–Pannonia) block and European plate. The strongly deformed slices of
M. Zielińska
semanticscholar +1 more source
JURASSIC PALEOGEOGRAPHY OF THE PIENINY AND OUTER CARPATHIAN BASINS
Rivista Italiana di Paleontologia e Stratigrafia, 2004 The Jurassic history of the Pieniny/Outer Carpathian basins reflects the evolution of the Circum-Tethyan area, especially its Alpine Tethys part. The Alpine Tethys that is Ligurian, Penninic Oceans and Pieniny/Magura Basin constitute the extension of the
JAN GOLONKA, MICHAL KROBICKI
doaj +1 more source
Geologica Carpathica, 2018 The Manín Unit represents a transitional tectonic element between the Central Western Carpathians and the Pieniny Klippen Belt. The overall map-view structure of the Manín Unit is dominated by elliptical antiforms composed of comparatively competent ...
Plašienka Dušan +2 more
doaj +1 more source
Thin‐Sheet Inversion Modeling of Geomagnetic Deep Sounding Data Using MCMC Algorithm
International Journal of Geophysics, Volume 2013, Issue 1, 2013., 2013 The geomagnetic deep sounding (GDS) method is one of electromagnetic (EM) methods in geophysics that allows the estimation of the subsurface electrical conductivity distribution. This paper presents the inversion modeling of GDS data employing Markov Chain Monte Carlo (MCMC) algorithm to evaluate the marginal posterior probability of the model ...
Hendra Grandis +3 more
wiley +1 more source