On the basis of triangular measurements done in 1954 and GPS measurements done in 1994 the neotectonic shifts along Orliśki fault were determinated. These measurements were used by Gelogogists who have determined the stabile points for the future measurements. Measurement points have been stabilised on the new way. Ali directions and distances in the net have been determined. Up to now three measuremts were completed. On the basis of the adjustmet the new coordinates have been obtained and by those the shifts along the Orliśki fault have been determined. The GPS geodynamic net was also stabilised and observed. This net covers the whole environment of the Krsko valley. Unfortunatelly, only the zero measurement was observed so far.
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In the seventies, seismological studies in Slovenia were complemented by geodetic measurements. The measuring instruments, measuring methods and data-processing algorithms employed have enabled conclusions on the stability or nonstability of a specific area in sometimes a relative short time periods. Geodetic networks have been set up along tectonic faults and are located in the most interesting parts of Slovene territory. Changes in the positions of network points are determined on the basis of terrestrial measurements performed in selected time intervals. Recently, these standard measurements have been joined and complemented by GPS measurements.This contribution presents the development of geodetic measurements of tectonic movements in Slovenia from 1977 to the present. Extremely precise measurements, which frequently do no receive sufficient (financial) support, are able to confirm the stability or nonstability of an observed area and complement seismological (geological) hypotheses and theories.
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In the seventies, seismological studies in Slovenia were complemented by geodetic measurements. The measuring instruments, measuring methods and data-processing algorihms employed have enabled conclusions on the stability or nonstability of a specific area in a relative short time periods. Geodetic networks have been set up along tectonic faults and are located in the most interesting parts of Slovene territory. Changes in the positions of network points are determined on the basis of terrestrial measurements performed in selected time intervals. Recently, these standard measurements have been joined and complemented by GPS measurements. The great further development of this activities were stimulated specially the cooperation in CERGOP I. This contribution presents the development of geodetic measurements of tectonic movements in Slovenia from 1977 to the present. Extremely precise measurements, which frequently do no receive sufficient (financial) support, are able to confirm the stability or nonstability of an observed area and complement seismological (geological) hypotheses and theories.
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The region of sub project Crustal Movements in the Eastern Alps and Northern Mediterranean is one of the most interesting geodynamic areas. There were a lot of very strong earthquakes in Europe. Therefore was already some local network stabilised and observed. In frame of CERGOP 2 is established WP 10.1. Presented is in tectonics of central region; Slovenia and Istria. on base of uphill now measurements was selected some point covering all region.
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Slovenia is situated in a region with strong earthquakes. In addition to international cooperation in CERGOP II, local measurements of recent movements are performed in Slovenia. The results of measurements of large power locations, i.e. of Coal Mine and Steam Power Station Velenje and Nuclear Power Station Krsko, are presented.
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Slovenia is situated in a region with strong earthquakes. In addition to international cooperation in CERGOP II, local measurements of recent movements are performed in Slovenia. The results of measurements of large power locations, i.e. of Coal Mine and Steam Power Station Velenje and Nuclear Power Station Krsko, are presented.
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The teritory of five countries is included in the project work: - Southern part of Austria and north east Italy, - Croatia, Bosnia and Hercegovina and Slovenia. For the purpose of harmonization of the activities we organised two meetings of representatives of these countries. First meeting was in Ljubljana but without representatives of Italy and Bosnia and Hercegovina. The second meeting was in Zagreb. The protocols of both meetings were send to the representatives of all countries. It was planed to geatherd the reports of all coutries but in this moment I can present only the report of activities in Slovenia.
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The region of sub project Crustal Movements in the Eastern Alps and Northern Mediterranean is one of the most interesting geodynamic areas. There were a lot of very strong earthquakes in Europe. Therefore was already some local network stabilised and observed. In frame of CERGOP 2 is established WP10.1. Presented is in tectonics of central region; Slovenia and Istria. On base of uphill now measurements was selected some point covering all region.