Results 21 to 30 of about 190,285 (154)
Geology and Geochemistry of Combustible MineralsIn presented article, on the basis of foraminiferal analysis and using the sedimentological data, the stratigraphy of the Upper Cretaceous deposits of the Pieniny Klippen Belt and the Marmarosh Klippen Zone is summarized and clarified, and the features of paleoceanography, in particular the paleobathymetry of sedimentatary basins, were reconstructed ...
Ksenia Navarivska, Oleh Hnylko
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17th EGU Émile Argand Conference on Alpine Geological StudiesThe extraordinary Western Carpathian tectonic structure, the Pieniny Klippen Belt (PKB), is characterized by its complex internal structure, particular tectonic units and a range of specific lithostratigraphic formations.
D. Plašienka +3 more
semanticscholar +2 more sources
The tectonics and stratigraphy of the transitional zone between the Pieniny Klippen Belt and Magura Nappe (Szczawnica area, Poland) [PDF]
, 2018 The Pieniny Klippen Belt is a narrow, complex structure stretching along a tectonic boundary between the Central and Outer Carpathians. Its formation involved two main evolutionary stages, the first, related to Late Cretaceous-Paleocene folding and ...
Edyta Jurewicz, Tomasz Segit
semanticscholar +3 more sources
Field trip - Outer Flysch Carpathians, Pieniny Klippen Belt (PKB), and Tatra Mountains
Geotourism/GeoturystykaThe 36th HKT Workshop (Himalaya-Karakorum- Tibet) is organised by the AGH University of Krakow, Poland. Kraków is situated at the front of the Carpathian orogenic system of the ancient Tethys Ocean and is perfect place for meeting between European-Asian Alpine-Himalayan orogenic belt with long history of the Western and Eastern Tethyan Ocean Realms ...
Michał Krobicki (ed.)
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Miocene transpression effects at the boundary of Central Carpathian Paleogene Basin and Pieniny Klippen Belt - examples from Polish-Slovakian borderland [PDF]
, 2018 A geological structural study has been conducted along the tectonic contact zone of the Central Carpathian Paleogene Basin (CCPB) and Pieniny Klippen Belt (PKB) in the eastern Podhale and western Spisska Magura areas.
M. Ludwiniak
semanticscholar +3 more sources
Foraminiferal assemblage in the coral-bearing limestones of the Vršatec area (Pieniny Klippen Belt, Western Carpathians, Slovakia) [PDF]
Geologica Carpathica, 2013 Abstract The paper deals with benthic foraminifera occurring with the scleractinian corals in the Jurassic biohermal and peribiohermal coral-bearing limestones of the Vršatec area (Czorsztyn Succession, Slovak Pieniny Klippen Belt). The coral community is dominated by branching forms of the genus Thecosmilia.
Morycowa, Elżbieta, Olszewska, Barbara
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Characteristics structures of the mélange zones in the Ukrainian Carpathians
Геофизический журнал, 2023 Mélange is characterized by the block-in-matrix fabric in which rigid blocks of different sizes, lithologies, and ages are distributed in a ductile matrix.
O. Hnylko, A. Murovskaya, M. Bohdanova
doaj +1 more source
Groundwater impact assessment of Lake Czorsztyn after 25 years of its operation [PDF]
Archives of Environmental Protection, 2022 Artificial water reservoirs pose impact on the natural environment. Impact of the artificial Czorsztyn Lake on groundwater and land management is assessed.
Włodzimierz Humnicki +5 more
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Basin Research, Volume 34, Issue 5, Page 1507-1535, October 2022., 2022 Mechanical accumulations of thin Bositra shells form mounds, with complex internal geometries (yellow dots), on the flat top of a drowned carbonate platform, lending an antiformal geometry to their Kimmeridgian–Tithonian drape (above dashed blue line).
Massimo Santantonio, Cristina Muraro
wiley +1 more source