Academic literature on the topic 'Carpathian-Pannonian Basin region'

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Journal articles on the topic "Carpathian-Pannonian Basin region"

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Bielik, M., Z. Alasonati-Tašárová, H. Zeyen, J. Dérerová, J. Afonso, and K. Csicsay. "Improved geophysical image of the Carpathian-Pannonian Basin region." Acta Geodaetica et Geophysica Hungarica 45, no. 3 (2010): 284–98. http://dx.doi.org/10.1556/ageod.45.2010.3.3.

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Bakk, Miklós. "The Boundaries of the Carpathian Basin – Frontiers and Regions." Acta Universitatis Sapientiae, European and Regional Studies 18, no. 1 (2020): 62–81. http://dx.doi.org/10.2478/auseur-2020-0011.

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Abstract The Carpathian Basin (or Pannonian Basin) is the south-eastern part of Central Europe, its geopolitical place being defined by geography (it is placed between the Eastern Alps, the Dinaric Alps, and the Carpathian Mountains) and from historical point of view by the fact that its core region was ruled for many centuries by the Hungarian Kingdom and the Habsburg Monarchy, and the neighbouring states aimed to extend their territories in the basin reducing the central role of the basin from the margins. The changes of the spatial domination in the Carpathian Basin created several centre–p
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Zsíros, T. "Earthquake magnitude relationships in the region of the Carpathian-Pannonian Basin." Acta Geodaetica et Geophysica Hungarica 47, no. 3 (2012): 358–76. http://dx.doi.org/10.1556/ageod.47.2012.3.6.

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Grinč, Michal, Hermann Zeyen, and Miroslav Bielik. "Automatic 1D integrated geophysical modelling of lithospheric discontinuities: a case study from Carpathian-Pannonian Basin region." Contributions to Geophysics and Geodesy 44, no. 2 (2014): 115–31. http://dx.doi.org/10.2478/congeo-2014-0007.

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Abstract Using a very fast 1D method of integrated geophysical modelling, we calculated models of the Moho discontinuity and the lithosphere-asthenosphere boundary in the Carpathian-Pannonian Basin region and its surrounding tectonic units. This method is capable to constrain complicated lithospheric structures by using joint interpretation of different geophysical data sets (geoid and topography) at the same time. The Moho depth map shows significant crustal thickness variations. The thickest crust is found underneath the Carpathian arc and its immediate Foredeep. High values are found in the
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Lakatos, Mónika, Tamás Weidinger, Lilla Hoffmann, Zita Bihari, and Ákos Horváth. "Computation of daily Penman–Monteith reference evapotranspiration in the Carpathian Region and comparison with Thornthwaite estimates." Advances in Science and Research 16 (February 20, 2020): 251–59. http://dx.doi.org/10.5194/asr-16-251-2020.

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Abstract. The Pannonian Basin Experiment (PannEx) is a Regional Hydroclimate Project (RHP) of the World Climate Research Programme (WCRP) Global Energy and Water Exchanges (GEWEX) Project. A gridded meteorological dataset is available for the PannEx region as part of the CarpatClim database, which consists of homogenized and harmonized daily meteorological observations for several climate parameters with 0.1∘ spatial resolution in the period of 1961–2010. The estimation of the Penman–Monteith reference evapotranspiration (ET0) on the daily scale was performed for the CarpatClim grid as one of
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Csicsay, Kristián, Miroslav Bielik, Andrej Mojzeš, Eva Speváková, Bibiána Kytková, and Michal Grinč. "Linearization of the Sobolev and Babeyko's formulae for transformation of P-wave velocity to density in the Carpathian-Pannonian Basin region." Contributions to Geophysics and Geodesy 42, no. 1 (2012): 15–23. http://dx.doi.org/10.2478/v10126-012-0002-y.

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Linearization of the Sobolev and Babeyko's formulae for transformation of P-wave velocity to density in the Carpathian-Pannonian Basin regionThe initial density model has to be based on a reasonable geological hypothesis and while the modelling process is non-unique, one of the interpretation aims is to define the robust parameters of the model. It is important at this stage to integrate the seismic and gravity data. One of the possibilities how to integrate these data is transformation of the seismic velocities to densities. The Sobolev and Babeyko's formulae belong to the most available rela
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Lillie, Robert J., Miroslav Bielik, Vladislav Babuška, and Jaroslava Plomerová. "Gravity modelling of the lithosphere in the Eastern Alpine-Western Carpathian-Pannonian Basin region." Tectonophysics 231, no. 4 (1994): 215–35. http://dx.doi.org/10.1016/0040-1951(94)90036-1.

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Hlavňová, Petra, Miroslav Bielik, Jana Dérerová, Igor Kohút, and Mariana Pašiaková. "A new lithospheric model in the eastern part of the Western Carpatians: 2D integrated modelling." Contributions to Geophysics and Geodesy 45, no. 1 (2015): 13–23. http://dx.doi.org/10.1515/congeo-2015-0010.

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Abstract Using 2D integrated geophysical modelling we recalculated lithospheric model along transect KP-X in the eastern part of the Western Carpathians. Our model takes into account the joint interpretation of the heat flow, free air anomalies, topography and geoid data. A more accurate model of lithospheric structure has been created, especially the lithosphere-astenosphere boundary. Lithosphere thickness in the study region increases from the area of the Pannonian Basin where we modelled it at the depth of 80 km towards the oldest and coolest area of the European Platform where it reaches a
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Petrescu, Laura, Graham Stuart, Gregory Houseman, and Ian Bastow. "Upper mantle deformation signatures of craton–orogen interaction in the Carpathian–Pannonian region from SKS anisotropy analysis." Geophysical Journal International 220, no. 3 (2020): 2105–18. http://dx.doi.org/10.1093/gji/ggz573.

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SUMMARY Since the Mesozoic, central and eastern European tectonics have been dominated by the closure of the Tethyan Ocean as the African and European plates collided. In the Miocene, the edge of the East European Craton and Moesian Platform were reworked in collision during the Carpathian orogeny and lithospheric extension formed the Pannonian Basin. To investigate the mantle deformation signatures associated with this complex collisional-extensional system, we carry out SKS splitting analysis at 123 broad-band seismic stations in the region. We compare our measurements with estimates of lith
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Šimonová, Barbora, and Miroslav Bielik. "Determination of rock densities in the Carpathian-Pannonian Basin lithosphere: based on the CELEBRATION 2000 experiment." Contributions to Geophysics and Geodesy 46, no. 4 (2016): 269–87. http://dx.doi.org/10.1515/congeo-2016-0016.

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Abstract The international seismic project CELEBRATION 2000 brought very good information about the P-wave velocity distribution in the Carpathian-Pannonian Basin litosphere. In this paper seismic data were used for transformations of in situ P-wave velocities to in situ densities along all profiles running across the Western Carpathians and the Pannonian Basin: CEL01, CEL04, CEL05, CEL06, CEL09, CEL11 and CEL12. The calculation of rock densities in the crust and lower lithosphere was done by the transformation of seismic velocities to densities using the formulae of Sobolev-Babeyko, Christens
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Dissertations / Theses on the topic "Carpathian-Pannonian Basin region"

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Grinc, Michal. "Lithospheric structure in Central Europe : integrated geophysical modelling." Phd thesis, Université Paris Sud - Paris XI, 2013. http://tel.archives-ouvertes.fr/tel-00921044.

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The main aim of this thesis is to gain new knowledge about the lithospherical structure and tectonics of the Carpathian-Pannonian Basin region. We applied three different methods: 1Dautomatic modelling, 2D integrated geophysical modelling and 3D inversion to achieve this goal.These methods are similar concerning the used databases but differ by used processing andinterpretation. At first we apply 1D automatic modelling to get a very first overview of thestudied region. Secondly, we apply 2D integrated modelling of the lithosphere which combines the interpretation of surface heat flow, geoid, g
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