Pregled bibliografske jedinice broj: 1068568
The fissure ridge of Abano Terme (Padova) and its seismic hazard implication
The fissure ridge of Abano Terme (Padova) and its seismic hazard implication // Atti del 29° Convegno Nazionale GNGTS, Tema 2: Caratterizzazione sismica del territorio
Prato, Italija, 2010. str. 201-203 (predavanje, međunarodna recenzija, kratko priopćenje, znanstveni)
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Naslov
The fissure ridge of Abano Terme (Padova) and its seismic hazard implication
Autori
Zampieri, Dario ; Pola, Marco ; Fabbri, Paolo
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, kratko priopćenje, znanstveni
Izvornik
Atti del 29° Convegno Nazionale GNGTS, Tema 2: Caratterizzazione sismica del territorio
/ - , 2010, 201-203
Skup
29° Convegno nazionale del Gruppo Nazionale di Geofisica della Terra Solida
Mjesto i datum
Prato, Italija, 26.10.2010. - 28.10.2010
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
travertine mound ; fracture mesh ; dilational step-over ; thermal waters ; Euganean Geothermal Field
Sažetak
This work details the results of the structural investigations performed on the Montirone travertine mound located in the Euganean Geothermal Field (Veneto region ; NE Italy). The travertine deposition is related to the natural outflow of thermal waters in the recent past. The mound is deformed by two fracture sets (WNW-ESE and NNE-SSW). They were interpreted as a fault/fracture mesh developing within the dilational stepover between strike-slip or transtensional fault segments of the regional Schio-Vicenza fault system. The presence of the Montirone travertine deposit strongly supports the existence of 1) a releasing structure in the subsurface which controls the development of the EGF, and 2) ongoing activity of the Schio-Vicenza fault, which places an urgent question about the seismic hazard of the area.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Rudarstvo, nafta i geološko inženjerstvo