Pregled bibliografske jedinice broj: 25037
Measuring strain and stress from sinkhole distribution, Example of the Velebit mountain range, Dinarides, Croatia.
Measuring strain and stress from sinkhole distribution, Example of the Velebit mountain range, Dinarides, Croatia. // Proceedings of the Seventh Multidisciplinary Conference on sinkholes and the engineering and environmental impacts on karst. / Beck, Barry F. ; Pettit, Arthur J. ; Herring, J. Gayle (ur.).
Rotterdam : Boston (MA) : Taipei: A.A. Balkema Publishers, 1999. str. 25-30 (predavanje, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
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Naslov
Measuring strain and stress from sinkhole distribution, Example of the Velebit mountain range, Dinarides, Croatia.
Autori
Faivre, Sanja ; Reiffsteck, Philippe
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Proceedings of the Seventh Multidisciplinary Conference on sinkholes and the engineering and environmental impacts on karst.
/ Beck, Barry F. ; Pettit, Arthur J. ; Herring, J. Gayle - Rotterdam : Boston (MA) : Taipei : A.A. Balkema Publishers, 1999, 25-30
Skup
Seventh Multidisciplinary Conference on sinkholes and the engineering and environmental impacts on karst
Mjesto i datum
Hershey (PA), Sjedinjene Američke Države; Harrisburg (PA), Sjedinjene Američke Države, 10.04.1999. - 14.04.1999
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
tectonic geomorphology; doline; stress; centre to centre method; method of projection; deformation rate; Velebit mountain range; Dinarides; Croatia.
Sažetak
The sinkholes appear to be a sensitive indicator of the recent tectonic activity. Their spatial distribution allows us the measurement of strain and stress to which the studied area has been submitted during recent periods. Our analysis is based on the center to center method (Ramsy, 1967 ; Fry, 1979), dealing with the determination of strain ellipse. This method is applied to the analysis of topographical changes in distribution of sinkholes. As a result we have obtained a considerable number of local results. To pass from a local to a regional level we have used Panozzos projection method (Panozzo, 1984). Both of these methods were adapted to the study of sinkholes. The results represent a very good base for the interpretation of recent local and regional deformation of the studied zone.
Izvorni jezik
Engleski
Znanstvena područja
Geografija
POVEZANOST RADA