Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Ľubomír Sliva"'
Autor:
Viktória Subová, Samuel Rybár, Katarína Šarinová, Natália Hudáčková, Michal Jamrich, Ľubomír Sliva, Branislav Šály, Ivan Hlavatý
Publikováno v:
Geologica Carpathica. 73
The Transcarpathian Basin, consisting of the Predov and Trebisov sub-basins, is situated at the border of the Western and Eastern Carpathians. Hydrocarbon exploration in this basin has been ongoing for more than 60 years and reserves of economic impo
Autor:
Tamás Csibri, Andrej Ruman, Natália Hlavatá Hudáčková, Michal Jamrich, Ľubomír Sliva, Katarína Šarinová, Michal Kováč
Publikováno v:
Geologica Carpathica. 73
Autor:
František Teťák, Ľubomír Sliva, Jozef Hók, Miroslav Bielik, Lenka Šamajová, Branislav Šály, Tamas Csibri, Bibiana Brixová
Publikováno v:
Geologica Carpathica, Vol 70, Iss 5, Pp 418-431 (2019)
The Vienna Basin is situated at the contact of the Bohemian Massif, Western Carpathians, and Eastern Alps. Deep borehole data and an existing magnetotelluric profile were used in density modelling of the pre-Neogene basement in the Slovak part of the
Publikováno v:
Geologica Carpathica, Vol 69, Iss 5, Pp 467-482 (2018)
The Blatné Depression located in the NW part of the Danube Basin represents the northernmost sub-basins of the Pannonian Basin System. Its subsidence is associated with oblique collision of the Central Western Carpathians with the European platform,
Autor:
Ľubomír Sliva, Natália Hudáčková, Tomáš Vlček, Petronela Nováková, Michal Šujan, Samuel Rybár, Michal Kováč, Marianna Kováčová, Michal Jamrich, Juraj Franců, Katarína Šarinová
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 559:109892
Deep wells penetrated Cenozoic sedimentary record of two different basins: 1) Oligocene retro-arc basin which is buried under the 2) Miocene back-arc Danube Basin. This study is focused on biotic and abiotic proxies discussed in terms of existing bio
Publikováno v:
Geologica Carpathica. 61:211-225
Reconstruction of Cenozoic paleostress fields and revised tectonic history in the northern part of the Central Western Carpathians (the Spišská Magura and Východné Tatry Mountains)This study investigates the chronology of paleostress evolution an
Autor:
Ľubomír Sliva, Eva Halásová, Aida S. Grigorovich, Michal Kováč, Peter Joniak, Martin Sabol, Rastislav Vojtko, Natália Hudáčková, Marianna Slamková, Ivan Baráth, Klement Fordinál
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 238:32-52
The Danube Basin situated at the Alpine–Carpathian–Pannonian junction represents a region of the Central Paratethys strongly influenced by orogen building processes and climatic changes. The geodynamic development mirrors gentle docking of the Ca