prikaz prve stranice dokumenta Constraints on complex faulting during the 1996 Ston–Slano (Croatia) earthquake inferred from the DInSAR, seismological, and geological observations
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Constraints on complex faulting during the 1996 Ston–Slano (Croatia) earthquake inferred from the DInSAR, seismological, and geological observations
Remote Sensing, 12 (2020), 7; 1157. https://doi.org/10.3390/rs12071157
Govorčin, Marin; Herak, Marijan; Matoš, Bojan; Pribičević, Boško; Vlahović, Igor

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Govorčin, M., Herak, M., Matoš, B., Pribičević, B. i Vlahović, I. (2020). Constraints on complex faulting during the 1996 Ston–Slano (Croatia) earthquake inferred from the DInSAR, seismological, and geological observations. Remote Sensing, 12. (7). doi: 10.3390/rs12071157

Govorčin, Marin, et al. "Constraints on complex faulting during the 1996 Ston–Slano (Croatia) earthquake inferred from the DInSAR, seismological, and geological observations." Remote Sensing, vol. 12, br. 7, 2020. https://doi.org/10.3390/rs12071157

Govorčin, Marin, Marijan Herak, Bojan Matoš, Boško Pribičević i Igor Vlahović. "Constraints on complex faulting during the 1996 Ston–Slano (Croatia) earthquake inferred from the DInSAR, seismological, and geological observations." Remote Sensing 12, br. 7 (2020). https://doi.org/10.3390/rs12071157

Govorčin, M., et al. (2020) 'Constraints on complex faulting during the 1996 Ston–Slano (Croatia) earthquake inferred from the DInSAR, seismological, and geological observations', Remote Sensing, 12(7). doi: 10.3390/rs12071157

Govorčin M, Herak M, Matoš B, Pribičević B, Vlahović I. Constraints on complex faulting during the 1996 Ston–Slano (Croatia) earthquake inferred from the DInSAR, seismological, and geological observations. Remote Sensing [Internet]. 04.04.2020. [pristupljeno 01.04.2025.];12(7). doi: 10.3390/rs12071157

M. Govorčin, M. Herak, B. Matoš, B. Pribičević i I. Vlahović, "Constraints on complex faulting during the 1996 Ston–Slano (Croatia) earthquake inferred from the DInSAR, seismological, and geological observations", Remote Sensing, vol. 12, br. 7, Travanj 2020. [Online]. Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:154708. [Citirano: 01.04.2025.]

Za citiranje koristite ovu mrežnu adresu: https://urn.nsk.hr/urn:nbn:hr:169:154708
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Podaci o radu
Naslov (engleski)Constraints on complex faulting during the 1996 Ston–Slano (Croatia) earthquake inferred from the DInSAR, seismological, and geological observations
AutorMarin Govorčin
AutorMarijan Herak
AutorBojan Matoš
AutorBoško Pribičević
AutorIgor Vlahović
Autorova ustanovaSveučilište u Zagrebu
Geodetski fakultet
Autorova ustanovaSveučilište u Zagrebu
Prirodoslovno-matematički fakultet
Autorova ustanovaSveučilište u Zagrebu
Rudarsko-geološko-naftni fakultet
(Zavod za geologiju i geološko inženjerstvo)
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Geologija
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Geofizika
Znanstveno / umjetničko
područje, polje i grana		TEHNIČKE ZNANOSTI
Geodezija
Sažetak (engleski)
This study, involving remote sensing, seismology, and geology, revealed complex faulting during the mainshock of the Ston–Slano earthquake sequence (5 September, 1996, Mw = 6.0). The observed DInSAR interferogram fringe patterns could not be explained by a single fault rupture. Geological investigations assigned most of the interferogram features either to previously known faults or to those newly determined by field studies. Relocation of hypocentres and reassessment of fault mechanisms... Više provided additional constraints on the evolution of stress release during this sequence. Available data support the scenario that the mainshock started with a reverse rupture with a left-lateral component on the Slano fault 4.5 km ESE of Slano, at the depth of about 11 km. The rupture proceeded unilaterally to the NW with the velocity of about 1.5 km/s for about 11 km, where the maximum stress release occurred. DInSAR interferograms suggest that several faults were activated in the process. The rupture terminated about 20 km away from the epicentre, close to the town of Ston, where the maximum DInSAR ground displacement reached 38 cm. Such a complicated and multiple rupture has never before been documented in the Dinarides. If this proves to be a common occurrence, it can pose problems in defining realistic hazard scenarios, especially in deterministic hazard assessment. Sakrij dio sažetka
Ključne riječi (engleski)
Jezikengleski
Vrsta publikacijeZnanstveni rad - Izvorni znanstveni rad
Status objaveObjavljen
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeObjavljena verzija rada (izdavačev PDF)
Naslov časopisaRemote Sensing
Brojčani podacivol. 12, br. 7, 1157
e-ISSN2072-4292
DOIhttps://doi.org/10.3390/rs12071157
URN:NBNurn:nbn:hr:169:154708
Datum objave publikacije2020-04-04
ProjektŠifra: IP-2014-09-9666
Naziv (hrvatski): Velebit od vrha do dna - multidisciplinanro istraživanje seizmoloških značajki i tektonike područja Velebita
Naziv (engleski): Velebit top to bottom – multidisciplinary research linking seismological data and tectonics in the Mt. Velebit region
Kratica: VELEBIT
Voditelj: Marijan Herak
Pravna nadležnost: Hrvatska
Financijer: Hrvatska zaklada za znanost
Linija financiranja: Research Projects
URL dokumentahttps://www.mdpi.com/2072-4292/12/7/1157
Vrsta resursaTekst
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Imenovanje 4.0 međunarodna (CC BY 4.0)
Datum i vrijeme pohrane2025-02-28 11:44:48
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