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Variation of strain and stress on the Velebit mountain range calculated from a geomorphological marker


Faivre, Sanja; Prelogović, Eduard; Reiffsteck, P.
Variation of strain and stress on the Velebit mountain range calculated from a geomorphological marker // Geological Meeting on Dynamics of Ongoing Orogeny PANCARDI 2000 : Pannonian Basin, Carpathian and Dinaride Sytem : abstracts ; u: Vijesti Hrvatskoga geološkog društva 37 (2003) (1) 1-154 / Tomljenović, Bruno ; Balen, Dražen. ; Saftić, Bruno. (ur.).
Zagreb: Hrvatsko geološko društvo, 2000. str. 36-36 (predavanje, sažetak, znanstveni)


Naslov
Variation of strain and stress on the Velebit mountain range calculated from a geomorphological marker

Autori
Faivre, Sanja ; Prelogović, Eduard ; Reiffsteck, P.

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni

Izvornik
Geological Meeting on Dynamics of Ongoing Orogeny PANCARDI 2000 : Pannonian Basin, Carpathian and Dinaride Sytem : abstracts ; u: Vijesti Hrvatskoga geološkog društva 37 (2003) (1) 1-154 / Tomljenović, Bruno ; Balen, Dražen. ; Saftić, Bruno. - Zagreb : Hrvatsko geološko društvo, 2000, 36-36

Skup
Geological Meeting on Dynamics of Ongoing Orogeny PANCARDI 2000 : Pannonian Basin, Carpathian and Dinaride Sytem

Mjesto i datum
Dubrovnik, Hrvatska, 01.-03.10.2000.

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Neobjavljeni rad

Ključne riječi
Dolines; tectonic geomorphology; strain and stress; Velebit mountain; Croatia

Sažetak
The strong relation between dolines and geological structure allow us the calculation of strain and stress orientation from the spatial distribution of dolines. The centre to centre method and the Frys graphical technique have been adapted to the new conditions and applied to dolines. The spatial distribution of results is related to the doline density of the study area. Once the punctual calculations of the finite strain are done the integration from one point to another is necessary to explain the spatial variations through the studied zone. Therefore, those results represent a base for the creation of the strain and stress trajectory maps of the Velebit mountain range. To pass from the local to the regional scale the Panozzos method has been used. In this way we have obtained the principal strain and stress orientations for the main tectonic blocs of the Velebit mountain range.

Izvorni jezik
Engleski

Znanstvena područja
Geografija



POVEZANOST RADA


Projekt / tema
119352

Ustanove
Prirodoslovno-matematički fakultet, Zagreb