Results 51 to 60 of about 190,285 (154)
Electrical Resistivity Tomography (ERT) method was applied to study a fragment of the Pieniny Klippen Belt (PKB), which has been investigated for more than 100 years. The study area is located in the Spisz Pieniny Mountains of southern Poland. The PKB in
G. Bania +2 more
semanticscholar +1 more source
Abstract The Carpathian–Pannonian Region (CPR), including Austria, Slovakia, Hungary, Croatia, Serbia, Romania, and Ukraine, exhibits significant seismic activity, necessitating detailed crustal studies. Despite recent improvements in understanding CPR's crustal structure, it remains poorly known. Here, we applied improved autocorrelation of the P‐wave
Hari Ram Thapa, Gordana Vlahovic
wiley +1 more source
The Orava Basin is an intramontane depression filled with presumably fine-grained sediments deposited in river, floodplain, swamp and lake settings. The basin infilling constitutes a crucial record of the neoalpine evolution of the Inner/Outer Carpathian
Łoziński Maciej +2 more
doaj +1 more source
Kimmeridgian limestone (KL) strata are one best example of a peritidal carbonate that records palaeogeographic and palaeoclimate conditions in Eastern Pontide, Eastern Black Sea region. The KL strata are represented by well‐preserved dark grey lime‐mudstones that archive important geochemical proxy.
Merve Özyurt, M. Ziya Kırmacı
wiley +1 more source
Upper Jurassic shallow-water scleractinian corals from the Pieniny Klippen Belt (Western Carpathians, Slovakia) [PDF]
Oxfordian shallow-water scleractinian coral association from the biohermal limestones of the Mt Vršatec (Czorsztyn Succession, Slovak sector of the Pieniny Klippen Belt, Western Carpathians) comprises 18 species (among them 2 new) plus 3 taxa determined
Morycowa, Elżbieta, Mišík, Milan
core
Abstract Unraveling the age and kinematics of low temperature deformation events is crucial in understanding the late‐stage evolution of orogens. However, accurate age constraints can often be challenging to obtain due to unideal outcrop conditions, large sedimentary hiatuses or the lack of well‐defined thermal events.
Éva Oravecz +7 more
wiley +1 more source
A hydrogeological study of springs in the western part of the Pieniny Klippen Belt, southern Poland [PDF]
The Pieniny Klippen Belt is characterised by diverse lithologies and complex tectonic strukture. The hydrogeological regime of sources can help in the recognition of regional hydrogeological conditions of this lithological-structural unit, as they ...
Żurawska, G.
core
Abstract Fold and thrust belt architecture may be influenced by basement geometry of the downgoing plate. This influence is notoriously difficult to assess due to a common lack of subsurface constraints and low resolution of exhumation estimates in space and time.
Bianca Heberer +7 more
wiley +1 more source
Deep-water benthic foraminifera were reported from lower Tithonian abyssal deposits lying above a barren interval of radiolarites in the Magura Basin (Western Carpathians).
ŠTEFAN JÓZSA
doaj +1 more source
Middle Jurassic stromatactis mud-mound in the Pieniny Klippen Belt (Western Carpathians)
A stromatactis mud-mound has been found near SlavnickeŽ Podhorie in the Czorsztyn Unit of the Pieniny Klippen Belt (Western Carpathians, Slovakia). Its stratigraphic range is Bathonian to Callovian and it is one of the youngest known true stromatactis mud-mounds.
Aubrecht, Roman +4 more
openaire +3 more sources

