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1
Content available remote Geodynamics of North Mediterranian and Eastern Alps
EN
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.
EN
Central Europe Regional Geodynamic Project (CERGOP) in Slovenia includes GPS measurements on 5 sites. Within the first part of the project during years 1994-1997, measurements were performed on one site (Ljubljana), and during the CERGOP-2 extension in years 1999-2005 additional 4 sites were added (Božica, Malija, Snežnik and Mrzlica). However, till now measurements on the three sites only (Ljubljana, Božica and Malija) have been completed. Obtained data show similar sense and amount of horizontal displacements. They exhibit general northward movement of sites at the average velocity of 3 mm/yr. This is in accordance with results obtained from other sites of cirkum-Adriatic region, and it confirms the northward movement of the Adriatic microplate towards the “stable” Eurasian plate. In Slovenia, a northward oriented δ1 tensor have been also obtained from several tens of earthquake fault plane solution. Slight defferences in sense and velocity of displacements among particular sites could be explained by the influence of local structures. In Slovenia, they belong to the Periadriatic dextral shear zone, to the Dinaric dextral shear zone, and to the Transdanubian sinistral shear zone. However, the real dynamics of particular structures, among which some also express co-seismic creep, will be possible to determine only by GPS measurements over a denser network of sites.
EN
Central Europe Regional Geodynamic Project (CERGOP) in Slovenia includes GPS measurements on 5 sites. Within the first part of the project during years 1994-1997, measurements were performed on one site (Ljubljana), and during the CERGOP-2 extension in years 1999-2005 additional 4 sites were added (Bozica, Malija, Sneznik and Mrzlica). However, till now measurements on the three sites only (Ljubljana, Bozica and Malija) have been completed. Obtained data show similar sense and amount of horizontal displacements. They exhibit general northward movement of sites at the average velocity of 3 mm/yr. This is in accordance with results obtained from other sites of circum-Adriatic region, and it confirms the northward movement of the Adriatic microplate towards the "stable" Eurasian plate. In Slovenia, a northward oriented Q] tensor have been also obtained from several tens of earthquake fault plane solution. Slight differences in sense and velocity of displacements among particular sites could be explained by the influence of local structures. In Slovenia, they belong to the Periadriatic dextral shear zone, to the Dinaric dextral shear zone, and to the Transdanubian sinistral shear zone. However, the real dynamics of particular structures, among which some also express co-seismic creep, will be possible to determine only by GPS measurements over a denser network of sites.
4
Content available remote Determination of local recent movements in Slovenia
EN
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.
EN
Central Europe Regional Geodynamic Project (CERGOP) in Slovenia includes GPS measurements on 5 sites. Within the first part of the project during years 1994-1997, measurements were performed on one site (Ljubljana), and during the CERGOP-2 extension in years 1999-2005 additional 4 sites were added (Bozica, Malija, Sneznik and Mrzlica). However, till now measurements on the three sites only (Ljubljana, Bozica and Malija) have been completed. Obtained data show similar sense and amount of horizontal displacements. They exhibit general northward movement of sites at the average velocity of 3 mm/yr. This is in accordance with results obtained from other sites of circum-Adriatic region, and it confirms the northward movement of the Adriatic microplate towards the "stable" Eurasian plate. In Slovenia, a northward oriented Ol tensor have been also obtained from several tens of earthquake fault pIane solution. Slight differences in sense and velocity of displacements among particular sites could be explained by the influence of local structures. In Slovenia, they belong to the Periadriatic dextral shear zone, to the Dinaric dextral shear zone, and tothe Transdanubian sinistraI shear zone. However, the real dynamics of particular structures, among which some also express co-seismic creep, will be possible to determine only by GPS measurements over a den ser network of sites.
6
Content available remote Determination of local recent movements in Slovenia
EN
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.
7
Content available remote Determination of local recent movements in Slovenia
EN
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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