Results 1 to 10 of about 98 (72)
Geology of the Magura Nappe, south-western Gorce Mountains (Outer Carpathians, Poland) [PDF]
Journal of Maps, 2021 The studied area, located in the south-western part of the Gorce Mountains, is built of flysch deposits representing the Krynica and Bystrica Subunits of the Magura Nappe.
Mateusz Szczech, Marek Cieszkowski
exaly +4 more sources
Structure and dynamics of deep-seated slope failures in the Magura Flysch Nappe, outer Western Carpathians (Czech Republic) [PDF]
Natural Hazards and Earth System Sciences, 2004 Deep-seated mass movements currently comprise one of the main morphogenetic processes in the Flysch Belt of the Western Carpathians of Central Europe. These mass movements result in a large spectrum of slope failures, depending on the type of movement ...
Ivo Baron, Rostislav Melichar
exaly +7 more sources
Alternative interpretation of the Bystrica Unit in Klanečnica KLK-1 borehole (Magura Nappe)
Mineralia SlovacaIn 1986, the KLK-1 (Klanečnica) borehole was drilled northwest of Moravské Lieskové as part of a regional oil and gas exploration programme. The well reached a total depth of 662 m and was intended to verify the occurrence and potential accumulation of ...
František Teťák +2 more
exaly +4 more sources
Numerical analysis of deep-seated mass movements in the Magura Nappe; Flysch Belt of the Western Carpathians (Czech Republic) [PDF]
Natural Hazards and Earth System Sciences, 2005 Deep-seated slope failures are common features in the mountains of the Raca Unit, Magura Nappe of the Flysch Belt of Western Carpathians. Since they represent very complicated system, understanding of their evolution and triggers still remains unclear ...
Ivo Baron +2 more
exaly +7 more sources
Central European Variscan Basement in the Outer Carpathians: A Case Study from the Magura Nappe, Outer Western Carpathians, Poland [PDF]
Minerals (Basel, Switzerland), 2021 Exotic crystalline blocks within the Outer Carpathian flysch have the potential to establish the nature of their eroded basement source(s) and thus to reconstruct the paleogeography of the Outer Carpathians. Petrological investigations (including mineral analyses) coupled with zircon and apatite U-Pb dating were performed on an exotic crystalline block
Aleksandra Gawęda +2 more
exaly +4 more sources
Geologica Carpathica, 2010 The gravity flow dynamics of submarine fan sedimentation in the Magura Basin of the Western Carpathians (Magura Nappe, Slovakia)This article deals with the dynamics of the deep-water gravity flows sedimentation within the Magura Formation. This investigation is based on analysis of the Magura sandstone sedimentary structures studied on the outcrops ...
František Teťák
exaly +2 more sources
Acta Geologica Hungarica, 2005 The Magura Nappe is the innermost tectonic unit of the Western Flysch Carpathians and is linked with the Rheno-Danubian flysch of the Eastern Alps. Toward the east this unit runs as an arc from Austria through the Czech Republic, Slovakia and Poland, and then narrows in Eastern Slovakia before disappearing east of Uzhhorod (Trans-Carpathian Ukraine ...
Nestor Oszczypko +1 more
exaly +4 more sources
Paleogene of the Magura Nappe adjacent to the Pieniny Klippen Belt between Szczawnica and Krościenko (Outer Carpathians, Poland) [PDF]
Geology Geophysics & Environment, 2014 The present authors investigated the Paleogene deposits of the internal zone of the Magura Basin known as Krynica Subunit or Krynica Zone in Poland. These deposits crop out in the peri-Pieniny zone, in area between Szczawnica and Krościenko. The oldest flysch deposits belong to the Paleocene – Lower Eocene Szczawnica Formation.
Jan Golonka, Anna Waśkowska-Oliwa
exaly +2 more sources
Geologica Carpathica, 2011 Stratigraphy and tectonics of a tectonic window in the Magura Nappe (Świątkowa Wielka, Polish Outer Carpathians)The Świątkowa Wielka Tectonic Window belongs to the Grybów Nappe of the Fore-Magura Group of units. This tectonic window is located in the marginal part of the Magura Nappe and is composed of Oligocene — Sub-Grybów Beds as well as the Grybów ...
Marta Oszczypko-Clowes +1 more
exaly +3 more sources
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 +2 more
doaj +3 more sources