Results 191 to 200 of about 19,454 (237)

Deep Seismic Lines of the Western Carpathians

60th EAGE Conference and Exhibition, 1998
In 1995 we have started a preparation of a project for producing of the Atlas of deep seismic lines of the Western Carpathians. This Atlas will be the first monographic work, in which more than 1000 km of profiles with regisfration up to 12 and 16 sec. will be processed in a complex way.
J. Santavy, V. Szalaiová, J. Vozár
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Lower Cretaceous carbonate platform facies, Western Carpathians

Palaeogeography, Palaeoclimatology, Palaeoecology, 1994
Abstract Two principal belts with “Urgonian” carbonate platform sedimentation evolved during the Barremian-Early Albian in the Western Carpathians. The northern grew on an accretionary belt in the convergence zone between the external and internal units. The limestones here contain rich ophiolite detritus.
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Mountain landscape archetypes of the Western Carpathians (Slovakia)

Biodiversity and Conservation, 2015
The concept of landscape archetypes arises from the idea of complex spatial structures allocation in the hierarchical and logical sequence, from the higher level to the lowest one (Hresko et al. Ekologia (Bratislava) 29:158–173, 2010). The landscape units being allocated on the basis of horizontal references of the secondary landscape structure are ...
J. Hreško, F. Petrovič, R. Mišovičová   +2 more
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Glacial-relict symptoms in the Western Carpathian flora

Folia Geobotanica, 2018
Glacial relicts have been regionally more common in glacial than in recent times. A rigorous assessment of which species are indeed glacial relicts is extremely difficult because direct evidence is untraceable or equivocal for many species. We aimed to identify species of the Western Carpathian flora (vascular plants, bryophytes and terrestrial lichens)
Daniel Dítě, Michal Hájek, Ivana Svitková, Alica Košuthová, Rudolf Šoltés, Ján Kliment   +5 more
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Epithermal Mineralization of the Western Carpathians

1999
Abstract km 0 The first Shell gas station on the M3 motorway after the end of Budapest sign. From here, the M3 motorway crosses the Gödöllő Hills during the next 35–40 kilometers. This area consists of a 2 km thick Tertiary-Quaternary sedimentary sequence underlain by Mesosoic carbonate rocks.
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Late Tertiary paleogeographic evolution of the Western Carpathians

Tectonophysics, 1993
Abstract The evolution of the Tertiary basins in the Western Carpathians was closely connected with the evolution of the Carpathian orogenic belt. During the Oligocene, the sea of the Outer Carpathian flysch troughs became for the first time part of the Paratethys regime due to isolation from the Mediterranean Tethys.
Michal Kováč, András Nagymarosy, Ján Soták, Katarína Šutovská   +3 more
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Flammulina fennae Bas in the Western Carpathians.

Česká Mykologie, 1987
The fungus Flammulina fennae is reported for the first time from Slovakia and the Carpathians. Comparison with the closely related Flammulina velutipes is provided, with distinctions in ecology and morphology, especially in spore size and stipe characteristics.
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Carex vaginata — new species in the Western Carpathians

Biologia, 2011
The first locality of Carex vaginata Tausch from the Western Carpathians is reported. This glacial relic was found at a refugial site in the Mt. Kubinska hoľa (the Oravska Magura Mts, Slovakia), in the saddle peat bog at 1,312 m a.s.l.
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Stratiform copper deposits of the western Carpathians, Czechoslovakia

Economic Geology, 1976
The Caledonian, Variscan, and Alpine metallogenic epochs of the western Carpathians are characterized by typomorphic minerals forming different types of deposits in various geological formations. The metals involved include Mg, Fe, Mn, Cu, Pb, Zn, Ag, Au, Hg, and Sb (Ilavsky and Cillik, 1959; Slavik et al., 1967; Varcek, 1967; Ilavsky, 1968).Stratiform
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Strain partitioning along the western margin of the Carpathians

Tectonophysics, 1998
Abstract Four profiles across the obliquely convergent West Carpathian external zone, together with a field study of the area, indicate the interrelation of thrusting and strike-slip faulting in the transpressionally deformed wedge. In the front of the wedge, thrusting is dominant.
M. Nemcok, J.J. Houghton, M.P. Coward
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