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A. Caporali C. Aichhorn M. Becker I. Fejes L. Gerhatova D. Ghitau G. Grenerczy J. Hefty S. Krauss D. Medak G. Milev M. Mojzes M. Mulic A. Nardo P. Pesec T. Rus J. Simek J. Sledzinski M. Solaric G. Stangl F. Vespe G. Virag F. Vodopivec F. Zablotskyi 《Journal of Geodynamics》2008,45(4-5):246-256
The Central European Geodynamics Project CERGOP-2, funded by the European Union from 2003 to 2006 under the 5th Framework Programme, benefited from repeated measurements of the coordinates of epoch and permanent GPS stations of the Central European GPS Reference Network (CEGRN), starting in 1994. Here we report on the results of the systematic processing of available data up to 2005. The analysis has yielded velocities for some 60 sites, covering a variety of Central European tectonic provinces, from the Adria Indenter to the Tauern Window, the Dinarides, the Pannonian Basin, the Vrancea Seismic Zone and the Carpathian Mountains. The estimated velocities define kinematical patterns which outline, with varying spatial resolution depending on the station density and history, the present-day surface kinematics in Central Europe. Horizontal velocities are analyzed after removal from the ITRF2000 estimated velocities of a rigid rotation accounting for the mean motion of Europe: a 2.3 mm/year north–south oriented convergence rate between Adria and the Southern Alps that can be considered to be the present-day velocity of the Adria Indenter relative to the European Foreland. An eastward extrusion zone initiates at the Tauern Window. The lateral eastward flow towards the Pannonian Basin exhibits a gentle gradient from 1 to 1.5 mm/year immediately east of the Tauern Window to zero in the Pannonian Basin. This kinematic continuity implies that the Pannonian plate fragment recently suggested by seismic data does not require a specific Eulerian pole. On the southeastern boundary of the Adria microplate, we report a velocity drop from 4 to 4.5 mm/year motion near Matera to 1 mm/year north of the Dinarides, in the southwestern part of the Pannonian Basin. A positive velocity gradient as one moves south from West Ukraine across Rumania and Bulgaria is estimated to be 2 mm/year on a scale of 600–800 km, as if the crust were dragged by the counterclockwise rotation along the North Anatolian Fault Zone. This regime apparently does not interfere with the Vrancea Seismic Zone: earthquakes there are sufficiently deep (>100 km) that the brittle deformation at depth can be considered as decoupled from the creep at the surface. We conclude that models of the Quaternary tectonics of Central and Eastern Europe should not neglect the long wavelength, nearly aseismic deformation affecting the upper crust in the Romanian and Bulgarian regions. 相似文献
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Three triangulation and trilateration micro networks in the seismic region of Ljubljana city, for the determination of horizontal and vertical movements, have been measured for the fourth time. GPS measurements have been included into the networks for the first time. The problem of the distance measurements was solved with the precise distancemeter Kern Mekometer ME 5000, angle measurements have been done with the electronic theodolite Kern E2. The problem of the orientation of the separated local networks was solved with GPS measurements. The results show that displacement in all three nets are not in the direction of the local fault but in the direction of the Sava fault and at the same time in the direction of the edge of the Peradriatic plate. 相似文献
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