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1
Content available remote Present-day Horizontal Mobility in the Serbian Part of the Pannonian Basin; Inferences from the Geometric Analysis of Deformations
Susić Z., Toljić M., Bulatović V., Ninkov T., Stojadinović U.
Acta Geophysica
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2016
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Vol. 64, no. 5
1626--1654
EN
In tectonically complex environments, such as the Pannonian Basin surrounded by the Alps–Dinarides and Carpathians orogens, monitoring of recent deformations represents very challenging matter. Efficient quantification of active continental deformations demands the use of a multidisciplinary approach, including neotectonic, seismotectonic and geodetic methods. The present-day tectonic mobility in the Pannonian Basin is predominantly controlled by the northward movement of the Adria micro-plate, which has produced compressional stresses that were party accommodated by the Alps-Dinarides thrust belt and partly transferred towards its hinterland. Influence of thus induced stresses on the recent strain field, deformations and tectonic mobility in the southern segment of the Pannonian Basin has been investigated using GPS measurements of the horizontal mobility in the Vojvodina area (northern Serbia).
2
Content available remote Late Miocene depositional units and syn-sedimentary deformation in the western Pannonian basin, Hungary
Fodor L I, Sztanó O, Magyar I, Törő B, Uhrin A, Varkonyi A, Csillag G, Kover S, Lantos Z, Nemeth A, Palotai M, Tokes L
Geologia Sudetica
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2014
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Vol. 42
14--15
3
Content available Lingula dregeri (Brachiopoda) from the Middle Miocene of Hungary
Bitner M. A., Dulai A., Kocsis L., Müller P. M.
Annales Societatis Geologorum Poloniae
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2012
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Vol. 82, No. 1
39–-43
EN
Lingulide brachiopods, assigned to Lingula dregeri Andreae, 1893, have been identified from the Middle Miocene (Upper Badenian) of the Hungarian part of the Pannonian Basin. Although widely distributed in the Miocene of the Central Paratethys (Austria, Poland, Ukraine, Romania), the genus Lingula was not described previously from Hungary. Outside of the Central Paratethys, L. dregeri also has been recognized in the Atlantic and Mediterranean provinces and most probably in the Eastern Paratethys.
4
Content available remote The motion of Adria and its effects on the Pannonian Basin: report of CERGOP-2/Enviroment WP10.3
Grenerczy G.
Reports on Geodesy
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2006
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z. 4/79
137-144
EN
The Central Europe Geodynamics Project (CERGOP) was initiated in 1993 [Fejes et al., 1993] and continued in 1995 as a European Union (EU) supported program. In 2003 the CERGOP-2/Environment Project, the successor of CERGOP, was commenced [Pesec, 2002]. The undertaken work in the CERGOP-2/Environment Project are shared and distributed to work packages. The work packages lO.x are formed to serve the main scientific users of the Central European GPS Geodynamic Reference Network (CEGRN) data. The work package 10.3 is devoted to integrate those geological and geophysical data that have primary importance regarding the present-day geodynamics of the Pannonian basin and its surroundings from the Adriatic microplate to the Carpathian Arc. This report is given about the works carried out between September 2003 and March 2004.
5
Content available remote Local geodynamic researches in Sudetes and the Mediterranean Region
Cacoń S., Kontny B., Bosy J., Cello G., Piccardi L, Tondi E., Drakatos G., Ganas A.
Reports on Geodesy
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2006
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z. 4/79
333-346
EN
The general characteristics of local tectonic movements studies basing on the self-developed monitoring system are presented in the paper. The system has been installed on some selected objects in the Sudetes (e.g. "Snieznik Massif and "Dobromierz") and in the Mediterranean basin ("Gargano" and "Norcia" in Italy, "Kaparelli" in Greece). These research areas are located in zones characterised with different magnitudes of recent tectonic activity. The main attention is given to organisation standards of the research network and monitoring of movements using GPS. The accuracy analysis of repeated GPS observations with respect to tectonic movements detection is also presented.
6
Content available remote Integration of present geodynamic investigations in the Pannonian Basin WP10.3 for the period between march 2004 and march 2005
Grenerczy G.
Reports on Geodesy
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2006
|
z. 4/79
145-148
EN
The CERGOP-2/Environment Project [Pesec, 2002], the successor of CERGOP [Fejes et aL, 1993] has several work packages to share the operational and scientifc work. The work package 10.3 is devoted to integrate those geological and geophysical data that have primary importance regarding the present-day geodynamics of the Pannonian basin and its surroundings from the Adriatic microplate to the Carpathian Arc. This report is given about the works carried out between March 2004 and March 2005.
7
Content available remote Report of the WP10.3 "Integration of present geodynamic investigations in the Pannonian Basin" for the period between March 2004 and March 2005
Grenerczy G.
Reports on Geodesy
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2005
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z. 2/73
111-114
8
Content available remote The motion of Adria and its effects on the Pannonian Basin: report of CERGOP-2/Environment WP10.3
Grenerczy G.
Reports on Geodesy
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2004
|
nr 4/71
107--114
EN
The Central Europe Geodynamics Project (CERGOP) was initiated in 1993 [Fejes et al., 1993] and continued in 1995 as a European Union (EU) supported program. In 2003 the CERGOP-2/Environment Project, the successor of CERGOP, was commenced [Pesec, 2002]. The undertaken work in the CERGOP-2/Environment Project are shared and distributed to work packages. The work packages lO.x are formed to serve the main scientific users of the Central European GPS Geodynamic Reference Network (CEGRN) data. The work package 10.3 is devoted to integrate those geological and geophysical data that have primary importance regarding the present-day geodynamics of the Pannonian basin and its surroundings from the Adriatic microplate to the Carpathian Arc. This report is given about the works carried out between September 2003 and March 2004.
9
Content available remote The geodynamics of the area between Alps, Bohemian Massif and a western part of Polish platform
Vyskočil P., Śledziński J.
Reports on Geodesy
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2004
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nr 2/69
179--188
EN
The area of western border of the CEI member countries is created by different geological structures as a part of Easter Alps, Carpathians, Pannonian Basin, Bohemian Massif and eastern area of Polish platform. This area includes northern slopes of the Alps, their foredeep and contact with the Bohemian Massif, West Carpathians foredeep towards Bohemian Massif and a part of Polish platform, crossing area of Sudeten fault zone and T-T zone. The entire territory is covered by map of annual velocities of vertical movements as well as by network of GPS stations. In present paper the geodynamical properties of mentioned above territory are analysed and shortly discussed both in vertical and horizontal component. It should be added that the vertical movements are derived from repeated levelling performed before and after the World War II and 1995. The horizontal component is derived from satellite (GPS) measurements after 1994 (see Fig. 1).
10
Content available remote Strain rates, seismic activity and its temporal variations within the Pannonian Basin
Varga P., Bus Z., Kiszely M.
Reports on Geodesy
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2004
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nr 2/69
149--156
EN
The spatio-temporal patterns are used for the study of the intraplate seismicity of the Pannonian basin. The earthquake occurrence is connected to the strain rate values with the use of the Kostrov(1974) equation. It is shown that in the Pannonian basin the seismic rates are l0-7-l0-6. These values were derived from the local earthquake catalogues of the area of Komarom, Dunaharaszti (near Budapest) and Kecskemet. The method used in present study is based on combination of seismological and geodetic tools and it can be used in the future for the study of the seismic conditions of areas with reduced earthquake activity.
11
Content available remote Report of the WP10.3 integration of present geodynamic investigations in the Pannonian Basin
Grenerczy G.
Reports on Geodesy
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2004
|
nr 4/71
191--193
EN
The undertaken work in the CERGOP-2/Environment Project [Pesec, 2002), the successor of CERGOP [Fejes et al., 1993] is shared and distributed to work packages. The work packages 10.x are formed to serve the main scientific users of the Central European GPS Geodynamic Reference Network (CEGRN) data. The work package 10.3 is devoted to integrate those geological and geophysical data that have primary importance regarding the present-day geodynamics of the Pannonian basin and its surroundings from the Adriatic microplate to the Carpathian Arc. This report is given about the works carried out between September 2003 and September 2004.
12
Content available remote Huge contrasts of the lithospheric structure revealed by new generation seismic experiments in Central Europe
Guterch A., Grad M., Keller R. G.
Przegląd Geologiczny
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2004
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Vol. 52, nr 8/2
753-760
EN
Beginning in 1997, Central Europe, between the Baltic and Adriatic Seas, has been covered by an unprecedented network of seismic refraction experiments (Fig.1A). These experiments — POLONAISE’97, CELEBRATION 2000, ALP 2002, and SUDETES 2003—have only been possible due to a massive international cooperative effort. International Consortium consisted of more than 30 institutions from 16 countries in Europe and North America—Austria, Belarus, Canada, Croatia, Czech Republic, Denmark, Finland, Germany, Hungary, Lithuania, Poland, Russia, Slovakia, Slovenia, Turkey, and the United States. The majority of the recording instruments was provided by the IRIS /PASCAL Instrument Center and the University of Texas at El Paso (USA), the Geological Survey of Canada, and other countries. For example, in the CELEBRATION experiment, the total number was 1230 stations and 147 shot points located along seismic lines of a total length of about 9000 km. A large number of seismic sources and stations in all experiments means that besides 2-D approach along profiles, also 3-D approach could be implemented in data interpretation. Total length of seismic profiles in all experiments is about 20,000 km.
13
Auxiliary 3-D electromagnetic induction models for the mantle diaper in the Pannonian Basin
Hvozdara M., Vozar J.
Acta Geophysica Polonica
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2002
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Vol. 50, nr 4
645-657
EN
Results of numerical calculations for the time-harmonic EM induction in two-layer Earth which contains a three dimensional (3-D) well conducting block in the first layer are presented. For these calculations, a method of vector integral equations is used. The parameters of the model are selected in order to approximate the gross-structural model of the diaper below the Pannonian Basin. Profile curves and isoline patterns for various characteristics of EM field on the surface are presented.
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