Results 21 to 30 of about 1,578 (175)

Discussion of ‘Olistostromes of the Pieniny Klippen Belt, Northern Carpathians’

Geological Magazine, 2016
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 ...
D. Plašienka, J. Soták, R. Aubrecht, J. Michalík   +3 more
semanticscholar   +4 more sources

Heavy mineral analysis of the Upper Cretaceous to Lower Eocene synorogenic formations of the Pieniny Klippen Belt (Šariš Unit, eastern Slovakia): new data from the Jar-2 borehole (Jarmuta-Proč Fm.) and outcrops (Malinowa Fm.)

Mineralia Slovaca
The study presents new results of heavy mineral analyses including detrital garnet, tourmaline and Cr-rich spinel chemical compositions from the synorogenic Maastrichtian-Ypresian Jarmuta-Proč Fm. of the Šariš Unit of the Pieniny Klippen Belt, penetrated
Jozef Madzin, Dušan Plašienka
doaj   +2 more sources

Age and provenance of mica-schist pebbles from the Eocene conglomerates of the Tylicz and Krynica Zone (Magura Nappe, Outer Flysch Carpathians) [PDF]

Geologica Carpathica, 2016
During the Łate Cretaceous to Palaeogene, the Magura Basin was supplied by clastic material from source areas situated on the northern and southern margins of the basin, which do not outcrop on the surface at present.
Oszczypko Nestor, Salata Dorota, Konečný Patrik   +2 more
doaj   +3 more sources

Provenance of synorogenic deposits of the Upper Cretaceous–Lower Palaeogene Jarmuta–Proč Formation (Pieniny Klippen Belt, Western Carpathians)

Geologica Carpathica, 2019
The Pieniny Klippen Belt contains thickening and coarsening upwards synorogenic sedimentary successions witnessing the collision of the Oravic ribbon continent with the Central Carpathian orogenic wedge after the closure of the Vahic Ocean in the Late ...
Madzin Jozef, Plašienka Dušan, Méres Štefan   +2 more
doaj   +2 more sources

ERT field survey supported with numerical and analogue modeling applied to study a fragment of the Pieniny Klippen Belt (Spisz Pieniny Mountains, southern Poland)

Geological Quarterly
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, Włodzimierz Jerzy Mościcki, Jan Golonka   +2 more
semanticscholar   +2 more sources

Field trip - Outer Flysch Carpathians, Pieniny Klippen Belt (PKB), and Tatra Mountains

Geotourism/Geoturystyka
The 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 ...
Michał Krobicki (ed.)
semanticscholar   +2 more sources

Upper Jurassic shallow-water scleractinian corals from the Pieniny Klippen Belt (Western Carpathians, Slovakia) [PDF]

, 2005
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
Mišík, Milan, Morycowa, Elżbieta
core   +2 more sources

Foraminiferal assemblage in the coral-bearing limestones of the Vršatec area (Pieniny Klippen Belt, Western Carpathians, Slovakia) [PDF]

Geologica Carpathica, 2013
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).
Morycowa, Elżbieta, Olszewska, Barbara
core   +3 more sources

Trace fossil curvolithus from the middle Jurassic crinoidal limestones of the Pieniny Klippen Belt (Carpathians, Poland) [PDF]

, 2003
The trace fossil Curvolithus simplex has been described for the first time in carbonate facies: the Bajocian crinoidal limestones of the Pieniny Klippen Belt. Curvolithus is typical of the Cruziana ichnofacies.
Krobicki, Michał, Uchman, Alfred
core   +2 more sources

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