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Pregled bibliografske jedinice broj: 944988

Coseismic deformation analysis of the 1996 Ston– Slano (southern Croatia) ML 6.0 earthquake: preliminary results using DInSAR and geological investigations


Govorčin, Marin; Matoš, Bojan; Herak, Marijan; Pribičević, Boško; Vlahović, Igor
Coseismic deformation analysis of the 1996 Ston– Slano (southern Croatia) ML 6.0 earthquake: preliminary results using DInSAR and geological investigations // 9th International INQUA Workshop on Paleoseismology, Active Tectonics and Paleoseismology / Koukousioura, O. ; Chatzipetros, A. (ur.).
Possidi: INQUA, 2018. str. 87-90 (predavanje, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)


Naslov
Coseismic deformation analysis of the 1996 Ston– Slano (southern Croatia) ML 6.0 earthquake: preliminary results using DInSAR and geological investigations

Autori
Govorčin, Marin ; Matoš, Bojan ; Herak, Marijan ; Pribičević, Boško ; Vlahović, Igor

Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni

Izvornik
9th International INQUA Workshop on Paleoseismology, Active Tectonics and Paleoseismology / Koukousioura, O. ; Chatzipetros, A. - Possidi : INQUA, 2018, 87-90

Skup
9th International INQUA Workshop on Paleoseismology, Active Tectonics and Paleoseismology

Mjesto i datum
Possidi, Grčka, 25-27.06.2018

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
Ston–Slano earthquake, Croatia, DInSAR, interferogram, compressional stress field

Sažetak
The Dinarides, a NW-striking mountain chain along the eastern margin of the Adriatic plate, is the most seismically active zone in Croatia. Historical and instrumental records indicate ongoing tectonics concentrated within southern Dalmatia. Results of the DInSAR analysis of coseismic deformation and fault kinematics for the Ston–Slano 1996 ML 6.0 earthquake are presented. Constructed interferograms suggest concentric fringe pattern of coseismic ground displacements, with maximum uplift of 26 cm and subsidence of c. 8 cm in the Podimoć area, approximately 8 km NW of 1996 Ston–Slano earthquake epicentre. The kinematic analysis of shear joint/fault data indicate compressional/transpressional stress field with NE–SW and locally NW–SE trending SHmax, coinciding with the present stress field. Considering the location of microseismic epicentre, analyzed interferograms and fault kinematics suggest that the earthquake rupture probably started near Slano, and proceeded towards NW along a reverse fault situated in the Adriatic offshore.

Izvorni jezik
Engleski

Znanstvena područja
Geologija, Geofizika, Geodezija



POVEZANOST RADA


Projekt / tema
HRZZ-IP-2014-09-9666 - velebit od vrha do dna - multidisciplinanro istraživanje seizmoloških značajki i tektonike područja Velebita (Marijan Herak, )

Ustanove
Geodetski fakultet, Zagreb,
Prirodoslovno-matematički fakultet, Zagreb,
Rudarsko-geološko-naftni fakultet, Zagreb,
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