Results 31 to 40 of about 639 (105)
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
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Geologické práce. SprávyThe work presents maps of the selected regions of the western Slovak section of the Flysch Belt of the Western Carpathians, including the contact with the Klippen Belt, compiled by the author in the period from 2001 to 2023.
František Teťák
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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 ...
Oszczypko-Clowes, Marta +1 more
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EnergiesThe paper presents the geochemical characteristics of 26 selected oil seeps, more than half of which are remnants of old oil wells. The samples were collected from three tectonic units: the Magura, Silesian, and Skole units in the Polish part of the ...
Wojciech Bieleń +3 more
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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
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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 ...
Oszczypko, Nestor +3 more
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Praesphaerammina, a new genus of Cenozoic deep-water agglutinated foraminifera from the Carpathian flysch deposits [PDF]
, 2000 The genus Praesphaerammina Kaminski and Filipcscu is newly described based on a revision of the type species Cystammina subgaleata Vasicek 1947. The genus differs from the Holocene genus Sphaerammina Cushman 1910 emend.
Filipescu, S., Kaminski, M.A.
core
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 ...
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Sféroidné pieskovcové konkrécie v malcovskom súvrství v Hruštíne na Orave
Geologické práce. SprávyPrimary and secondary occurrences of larger sandstone spheroidal concretions (balls), which are not yet mentioned in professional or popular literature, were found in Hruštín village (Slovakia) and its surroundings during of detailed geological mapping ...
František Teťák
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Annales Societatis Geologorum Poloniae, 2017 The thin- and medium-bedded, turbiditic deposits that are exposed in the Bystrica Zone of the Magura Nappe in the Slovak Orava region are the subject of this study. On the basis of lithological features as well as age and stratigraphic position, they are assigned to the Ropianka Formation.
Teťák, František +4 more
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