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1
100%
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
2
80%
Folia Quaternaria
2003 nr 74 35-56
EN On the south slope of the pass between Kotoń Mt. and Pękalówka Mt. (Western Carpathians, Beskid Makowski Range), there occur big landslide with longitudinal deppressions, felt up of minerotrophic mire, with particularly long sequence of the Late Glacial deposits. The sediments were analysed by palyn[...]
3
80%
Folia Quaternaria
2003 nr 74 17-34
EN A depression within the small Kaletowa landslide, Beskid Makowski (Średni) Mts., Outer Carpathians, is filled with 1.8-m-thick organic-mineral sediments of a fen-type peatbog. Some radiocarbon datings using various material (wood detritus, tree trunk, organic silt) obtained from the bottom of the de[...]
4
80%
Folia Quaternaria
2003 nr 74 75-96
EN Successive phases of the Siekierczyna landslide evolution (the Beskid Wyspowy Mts., Outer West Carpathians) are related to Holocene climatic changes. Three phases of the landslide rejuvenation have been radiocarbon dated at: 3.8 ka, 2.9 ka and 2.2 ka. During these phases the valley of the Lasówka st[...]
5
80%
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
6
80%
Geology, Geophysics and Environment
EN The 15th International Conference of Young Geologists was held in the Polish Outer Carpathians, in Międzybrodzie Żywieckie, located in the Beskid Mały Mts. All participants were hosted in Niagara resort. The conference was organized by the AGH University of Sciences and Technology (AGH), Krakow (PL)[...]
7
80%
Biuletyn Państwowego Instytutu Geologicznego
2001 nr 396 152-153
8
80%
Studia Quaternaria
2007 Vol. 24 47-52
EN This paper presents the results of a detailed analysis of fractured clasts hosted within Miocene and Pleistocene paraconglomerates that are exposed close to a map-scale overthrust. Both these paraconglomerates bear numerous fractured clasts (22-50%). The architecture of fractures (joints and minor f[...]
9
80%
Geological Quarterly
EN The joint network in the portion of the Dukla Nappe studied originated in two stages showing different orientations of the stress field axes. The older, compressive stage I was characterised by a N45°E-orientated (at present coordinates) horizontal s1, and formation of the diagonal, shear (SL and SR[...]
10
80%
Journal of Ecological Engineering
2017 Vol. 18, nr 4 100--109
EN The Carpathians may play a significant role as a supplier of greenhouse gases to the atmosphere. Unfortunately, most of the discovered oil and gas deposits are recently only historical objects. An example is the Sękowa-Ropica Górna-Siary oil deposit located in the marginal part of the Magura Nappe w[...]
11
80%
Geological Quarterly
2017 Vol. 61, No. 1 214--226
EN Random vitrinite reflectance of allochthonous plant material varies throughout all the flysch sedimentary units of the Outer Western Carpathians. The vitrinite reflectance of coalified phytogenic matter is variable even within the same lithostratigraphic unit. There is no clear relationship between [...]
12
80%
Geotourism / Geoturystyka
2014 nr 1 3--14
EN The Klimkówka Lake geotouristic site is one of the greatest attractions of the Beskid Niski Mountains of the Polish Carpathians Mts. Nearly 20 years of existence of the artificial dam lake generated the development of tourism in the area. The great advantage of Klimkówka Lake region is the presence [...]
13
80%
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
14
80%
Annales Societatis Geologorum Poloniae
EN Semi-detailed magnetotelluric sur vey was carried out in the area between Kamienica Dolna, Gogołów and Łopuchowa in the Polish Outer Carpathians. Magnetotelluric soundings were made along three lines located in a zone of the tectonic loop in the Carpathians' basement, which is reflected by the distr[...]
15
70%
Geological Quarterly
2013 Vol. 57, No. 2 307–-324
EN Based on geochemical data of the Oligocene Menilite Shales in the Boryslav–Pokuttya, Skole (Skyba), Silesian (Krosno) and Dukla units in the Carpathians, between Krosno and Styi towns, 1D modelling of generation and expulsion processes of hydrocarbons has been carried out. These strata are character[...]
16
70%
Geological Quarterly
2012 Vol. 56, No. 4 833-–844
EN Three units of laminated coccolith limestone are used as regional chronohorizons in the Oligocene of the Outer Carpathians. Two of them – the Tylawa Limestones and the Jasło Limestone display a similar type of lamination and their discrimination is in some cases problematic. We provide a detailed me[...]
17
70%
Bulletin of the Polish Academy of Sciences. Earth Sciences
EN The present paper deals with the Upper Paleocene - Lower and Middle Eocene deposits in the Siary Subunit of the Magura Nappe in the area of Sucha Beskidzka, Polish Outer Carpathians. They are represented by variegated shales of the Łabowa Shale Formation intercalated with thick-bedded sandstones tra[...]
18
70%
Geological Quarterly
EN In the Nowy Sącz area Early Miocene marine deposits have been discovered in the southern part of the Rača Subunit, and at the front of the Bystrica Subunit of the Magura Nappe. These deposits belong to the Zawada Formation, which is represented by medium- to thick-bedded glauconitic sandstones with [...]
19
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Geological Quarterly
2014 Vol. 58, No. 2 337--352
EN Detrital fragments of automorphic tourmaline crystals are commonly incorporated in tests of simple agglutinated foraminifera that lived in the deep-marine Carpathian turbidite basin, in which deposition of the Hieroglyphic beds (Eocene) took place. Such grains were observed in the tests of 37 taxa r[...]
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Geological Quarterly
2017 Vol. 61, No. 3 682--695
EN During the Paleogene, the area of the northern Tethys was controlled by a turbidity system stimulated by diastrophic and geodynamic processes. These factors contributed to the dispersion and rapid oxygenation of organic debris. Its accumulation was a consequence of stagnant bottom water conditions t[...]
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