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Wyszukujesz frazę "Caporali, A." wg kryterium: Autor


Wyświetlanie 1-3 z 3
Tytuł:
New challenges for the CEGRN
Autorzy:
Caporali, A.
Powiązania:
https://bibliotekanauki.pl/articles/224916.pdf
Data publikacji:
2011
Wydawca:
Politechnika Warszawska. Wydział Geodezji i Kartografii
Tematy:
CEGRN
Opis:
The Central European Geodynamic Reference Network is active since the early 1990's with a consistent and systematic activity of measurement, processing and scientific interpretation of the GPS and derived data. The project CERGOP 2 which was financed by the EU under FP5 has contributed to build the necessary cohesion and awareness of the different fields of expertise which are necessary to manage a geodetic network spanning Central Europe, and with important connections to other networks, in particular the EPN. In this second decade there are a number of challenges which will need a strong effort. The ambitious EPOS and TopoEurope projects are looking for a homogeneous and consistent dense velocity field for application to geodynamics and seismicity. The theme of the dense velocity field is present also within the IAG, in the working group 'Regional Dense Velocity Fields'. Finally, the way in which the ETRF2000 coordinates of stations in national networks evolve relatively to the stable part of Europe is related to the details of the 3D velocities. This is relevant to INSPIRE, and the obligation of the EU Countries to follow the ETR89 standards. CEGRN has the potential to effectively play an active role in these scientific issue, because the CEGRN campaigns are of high quality, fulfill state-of-the-art standards and extend over a very long lapse of time. Possible initiatives linked to the scientific projects mentioned above include 1) a participation in the proposed COST Action called TEGO 'Towards a European GNSS Observatory'; 2) a study of the best way to combine the CEGRN campaign solutions with the EPN network solution.
Źródło:
Reports on Geodesy; 2011, z. 2/91; 9-18
0867-3179
Pojawia się w:
Reports on Geodesy
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geokinematics of Central Europe: new insights from CERGOP-2/Environment Project
Autorzy:
Caporali, A.
Becker, M.
Fejes, I.
Gerhatova, L.
Ghitau, D.
Grenerczy, G.
Hefty, J.
Medac, D.
Milev, G.
Mojzes, M.
Mulic, M.
Powiązania:
https://bibliotekanauki.pl/articles/224596.pdf
Data publikacji:
2007
Wydawca:
Politechnika Warszawska. Wydział Geodezji i Kartografii
Tematy:
GPS
geodezja
geodynamika w Europie Centralnej
tektonika w Europie Centralnej
naprężenia i odształcenia w Europie Środkowej
GPS Geodesy
Central European Geodynamics
Central European Tectonics
Stress and Strain in Central Europe
Opis:
The CERGOP2 project funded by the European Union from 2003 to 2006 under the 5th Framework Programme benefits from repeated measurements of the coordinates of epoch and permanent GPS stations forming the CEGRN network in Central Europe, starting 1994. We report on the results of the systematic processing of the available data up to 2005. The analysis work has yielded the velocities of some 60 sites, covering a variety of Central European tectonic provinces, from the Adria indenter to the Tauern window, 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 tectonic flow in Central Europe.The CEGRN data show that the majority of active contraction originating from the Eurasia Nubia plate boundary and the microplate between them is taken up primarily in the Eastern Alps, the Dinarides, and the Pannonian Basin. After removal from the ITRF2000 velocities of a rigid rotation accounting for the mean motion of stable Europe, the residual velocities have random orientations with 0.3 mm/yr scatter. This Iow figure provides an upper estimate for the level of rigidity of the European Platform. A 2.3 mm/yr north-south oriented convergence rate is implied by our data between Adria and the Southern Alps, and a narrow - -60 km wide- contraction zone in the Southern Alps is identified, consistently with earlier results. An eastward extrusion north of the contraction zone corresponds with the extension of the Tauern Window. In the southeastern boundary of the microplate, 4-4.5 mm/yr motion of Adria decreases to -1 mm/yr through the microplate, its boundary, and the Dinarides mountain range towards the southwestern part of the Pannonian Basin. Our data suggest that if the Pannonian Basin is subject to deformation, then it is most likely to be compressional than extensional. We conclude that compression and associated contraction due to the Adria collision with the Alps and the Dinarides is likely to fade away in the Western and Northern Carpathians, where our velocities and strain rates show no significant deformation.
Źródło:
Reports on Geodesy; 2007, z. 2/83; 7-46
0867-3179
Pojawia się w:
Reports on Geodesy
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geokinematics of Central Europe from GPS data
Autorzy:
Caporali, A.
Śledziński, J.
Powiązania:
https://bibliotekanauki.pl/articles/224784.pdf
Data publikacji:
2006
Wydawca:
Politechnika Warszawska. Wydział Geodezji i Kartografii
Tematy:
GPS projekt
geokinematyka
Europa
GPS project
geokinematics
Europe
Opis:
In several seismic or potentially seismic areas deformation processes at moderate depth generate deformation at the surface and measurement of such surface deformation is an important boundary condition to models of the evolution of interacting blocks before, during and after earthquakes. the network of some 160 permanent GPS stations disseminated in Europe under the European Permanent Network of EUREF and the CERGOP 2 Project of the European Union, with additional local densification stations, provides a valuable contribution to the estimate of the average surface strain rate. The expected strain rate is of the order of 20-40 nanostrian per year, corresponding to a velocity change of a few mm/year over distances of some hundreds of km. Consequently, we require accuracies in the velocities of fractions of mm/year and full control of systematic errors which may mask tectonic signals. Based on our systematic processing of GPS data from permanent European GPS stations covering nearly a decade (1995-2005) we present the large scale velocity flow across most of continental Europe and the associated horizontal gradient or strain rate field.
Źródło:
Reports on Geodesy; 2006, z. 2/77; 17-28
0867-3179
Pojawia się w:
Reports on Geodesy
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-3 z 3

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