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Izvorni znanstveni članak
https://doi.org/10.15291/geoadria.165

Remote sensing as a preliminary analysis for the detection of active tectonic structures: an application to the Albanian orogenic system

Andrea Favretto ; GIS Laboratory – University of Trieste
Riccardo Geletti ; The National Institute of Oceanography and Experimental Geophysics (OGS) - Trieste
Dario Civile ; The National Institute of Oceanography and Experimental Geophysics (OGS) - Trieste

Puni tekst: engleski, pdf (4 MB) str. 97-111 preuzimanja: 1.360* citiraj
APA 6th Edition
Favretto, A., Geletti, R. i Civile, D. (2013). Remote sensing as a preliminary analysis for the detection of active tectonic structures: an application to the Albanian orogenic system. Geoadria, 18 (2), 97-111. https://doi.org/10.15291/geoadria.165
MLA 8th Edition
Favretto, Andrea, et al. "Remote sensing as a preliminary analysis for the detection of active tectonic structures: an application to the Albanian orogenic system." Geoadria, vol. 18, br. 2, 2013, str. 97-111. https://doi.org/10.15291/geoadria.165. Citirano 21.04.2021.
Chicago 17th Edition
Favretto, Andrea, Riccardo Geletti i Dario Civile. "Remote sensing as a preliminary analysis for the detection of active tectonic structures: an application to the Albanian orogenic system." Geoadria 18, br. 2 (2013): 97-111. https://doi.org/10.15291/geoadria.165
Harvard
Favretto, A., Geletti, R., i Civile, D. (2013). 'Remote sensing as a preliminary analysis for the detection of active tectonic structures: an application to the Albanian orogenic system', Geoadria, 18(2), str. 97-111. https://doi.org/10.15291/geoadria.165
Vancouver
Favretto A, Geletti R, Civile D. Remote sensing as a preliminary analysis for the detection of active tectonic structures: an application to the Albanian orogenic system. Geoadria [Internet]. 2013 [pristupljeno 21.04.2021.];18(2):97-111. https://doi.org/10.15291/geoadria.165
IEEE
A. Favretto, R. Geletti i D. Civile, "Remote sensing as a preliminary analysis for the detection of active tectonic structures: an application to the Albanian orogenic system", Geoadria, vol.18, br. 2, str. 97-111, 2013. [Online]. https://doi.org/10.15291/geoadria.165

Sažetak
As is well known, both the traditional direct geological and geophysical survey methods used to identify geologic features are very expensive and time-consuming procedures.
In this regard, remote sensing methods applied to multispectral and medium spatial resolution satellite images allow a more focused approach with respect to the more specific geologic methods. This is achieved by a preliminary land inspection carried out by the semi-automated analysis of satellite imagery. This avoids wasting resources as the geological/geophysical survey methods can be later applied only to those zones suspected of having certain tectonic activity (derived by the remotely sensed imagery).
This paper will evaluate an ASTER sensor satellite image (and its derived Digital Elevation Model or DEM), in order to point out the suspected presence of active geologic structures (faults). The area in question is west – central Albania. The results of the remote sensing procedures are later compared with the established data for the same area taken by satellite images, in order to verify the reliability of the adopted method. The source of the established data has been from the bibliography.

Ključne riječi
active faults; remote sensing; ASTER; Albania

Hrčak ID: 118889

URI
https://hrcak.srce.hr/118889

[hrvatski]

Posjeta: 1.735 *