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1
Content available remote National Report of Slovakia 1994-1997
100%
Mojzes M.
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1998
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tom z. 10/40
85-88
2
Content available remote UNIGRACE National Report of Slovakia, 2nd UNIGRACE Working Conference, Warsaw, February 22-23, 1999
100%
Mojzes M.
|
1999
|
tom z. 2/43
75-82
3
Content available remote National Reort of Slovakia
100%
Mojzes M.
|
1998
|
tom z. 2/32
65-71
4
Content available remote Partner Progress Report from 1.1.1999 to 31.12.1999
100%
Mojzes M.
|
2000
|
tom z. 5/51
77-80
5
Content available remote Geodynamics of the Tatra Mountains - present status and future development of the project
63%
Mojzes M. , Czarnecki K.
|
2000
|
tom z. 7/53
123-124
6
Content available remote The Central Europe geodynamics project (CERGOP): main achievements 1995-1998
51%
Fejes D. , Ghitau C. , Marchesini M. , Mojzes M.
|
1998
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tom z. 9/39
21-38
EN
Tbe CentraI European Geodynamic Reference Network (CEGRN) based on GPS measuremnts bas been established consisting of 31 sites in 11 CentraI European countries. Four epoch measurements were carried out spanning 3 years from 1994-1997. The results of the yearly epoch measurements on the CEGRN are the basis for a number of studies. There are 11 permanent GPS stations operating in the area. Nine multinational CERGOP Study Groups (CSG) are active and some of their resuIts are presented here. The CERGOP Data Centre is functioning efficiently and smoothly in Graz, Austria. Processing of the observational data is carried out in tbe CERGOP Processing Centres (Bratislava, Frankfurt am Main, Graz, Matera, Pecny, Penc, Warsaw and Zagreb). The data analysis is done within CSG4. Important achievement is that the accuracy of the CEGRN epoch coordinates is on the sub-centimeter level. Based on CEGRN the Central European Terrestrial Reference Frame (CETRF) has been established as the result of activity of CSG3. Publication of the proceedings and results of the study groups is carried out by the Warsaw University of Technology, Poland, quickly and efficiently in the series REPORTS 0N GEODESY. We are aware of a number of local deformation studies in the participating countries where CEGRN sites are used as reference. CERGOP has integrated a considerable part of geodynamic research in Central Europe, established a large number of collaboration, exchange of information and perhaps most notably - mutual trust and understanding among the participants.
7
Content available remote Tatra Mountains without borders
51%
Czarnecki K. , Janak J. , Mojzes M.
|
1998
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tom z. 9/39
131-136
EN
The "Tatra Mountains without borders" is a local project ror studying 3D displacements of points located in Tatra Mountains comprising the Slovak-Polish border. The test-network consisting of 28 stations is devoted to study both local geoid and recent tectonic movements in this region. GPS network in different height levels for tropospheric studies.The first GPS measurement campaign was carried out in September 1997 and local quasigeoid from gravimetric, GPS and levelling data in this area was determined.
8
Content available remote Geodynamics of the Tatra Mountains
51%
Mojzes M. , Czarnecki K. , Cundrelik R.
|
2000
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tom z. 6/52
35-38
9
Content available remote New geodynamic project "Czech-Polish-Slovak cross-border studies of regional Geodynamics"
51%
Mojzes M. , Schenk V. , Śledziński J. , Vyskocil P.
|
2001
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tom z. 2/57
101-106
EN
Long borderline between Poland, Czech Republic and Slovakia coincides generally with very interesting geotectonic formations of different age that give an excellent opportunity to undertake a comparative studies that have a significant scientific and practical value. The main general objective of the Project is to investigate the variations of the recent crustal movements and periodic monitoring of the horizontal and vertical displacements in the structural active tectonic zones of the Polish and Czech parts of the Sudetes Mts. and the Western Carpathians as well as in the regions located close to the existing and planned investments and technical constructions (water reservoirs and dams, power stations, communication lines, etc.). In the Tatra Mts., that represent the youngest tectonic formation of the area of Central Europe, the tectonic movements and relativety significant velocity vectors will be monitoring as well as the location of the geoid (the quasi-geoid) related to the geocentric reference ellipsoid will be determined. The established test control networks in Sudetes Region and in Tatra Mts. will be used by Polish, Czech and Slovak geodesists and surveyors for testing new technologies and upgrading the practical quick methods of satellite and geodetic positioning procedures applicable for geodesy and navigation, in particular in hilly and mountainous areas. The project will be realised in the frame of the CEI CERGOP Study Group CSG.5 "Geotectonic analysis of the regions of Central Europe". 1. BACKGROUNDS AND OBJECTIYES OF THE PROJECT Long borderline between Poland, Czech Republic and Slovakia coincides generally with very interesting geotectonic formations of different agę that give an escellent opportunity to undertake a comparative studies that have a significant scientiflc and practical value. Mobility interrelations between two fundamenta! geological structures in Central Europę, which represent old platform and young orogenic formations, influence to whole European geodynamics. Geodynamical mobility monitored up-to-now
10
Content available remote CERGOP Study Group No 2: site quality monitoring, final report
45%
Levai P. , Borza T. , Fejes I. , Kujawa L. , Mojzes M.
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1998
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tom z. 10/40
115-135
11
Content available remote Testing of gravimetric quasigeoid by astronomical measurements
32%
Mojzes M. , Husar L. , Janak J. , Papco J. , Czarnecki K. , Barlik M. , Bogusz J. , Walo J.
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2006
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tom z. 4/79
203-211
EN
The current determination of quasigeoid is largely based on gravimetric observations, which in general do not cover areas equally. That causes decreasing in quality of quasigeoid determination in those areas that are sparsely covered (surveyed) by gravimetric measurements. This situation was occurred on territory of the Slovak Republic in the Tatra Mountains area where gravimetric observations were performed only in some valleys and crests and from Polish side were only applied average values of Bouguer gravity anomalies with a 5' x 7.5' grid spacing (10 km x 10 km) which were transformed to average free-air gravity anomalies. To testing precision of the determined gravimetric quasigeoid it's desirable to use independent method such as astronomical method. Essentially is concerned with comparison astronomical and gravimetric of vertical deflections in the given region and with modelling of the differences between astronomical and gravimetric vertical deflections.
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