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Muco, B.
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- PublicationOpen AccessSeismic hazard assessment for Adria(1999-12)
; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ;Slejko, D.; Osservatorio Geofisico Sperimentale, Trieste, Italy ;Camassi, R.; Gruppo Nazionale Difesa Terremoti c/o Università di Bologna, Italy ;Cecic, I.; Geophysical Survey of Slovenia, Ljubljana, Slovenia ;Herak, D.; Geophysical Institute, University, Zagreb, Croatia ;Herak, M.; Geophysical Institute, University, Zagreb, Croatia ;Kociu, S.; Seismological Institute, Tirana, Albania ;Kouskouna, V.; Department of Geophysics, University, Athens, Greece ;Lapajne, J.; Geophysical Survey of Slovenia, Ljubljana, Slovenia ;Makropoulos, K.; Department of Geophysics, University, Athens, Greece ;Meletti, C.; Gruppo Nazionale Difesa Terremoti c/o Università di Pisa, Italy ;Muco, B.; Seismological Institute, Tirana, Albania ;Papaioannou, C.; Institute of Engineering Seismology and Earthquake Engineering, Thessaloniki, Greece ;Peruzza, L.; Gruppo Nazionale Difesa Terremoti c/o Osservatorio Geofisico Sperimentale, Trieste, Italy ;Rebez, R.; Osservatorio Geofisico Sperimentale, Trieste, Italy ;Scandone, P.; Dipartimento di Scienze della Terra, Università di Pisa, Italy ;Sulstarova, E.; Seismological Institute, Tirana, Albania ;Voulgaris, N.; Department of Geophysics, University, Athens, Greece ;Zivcic, M.; Geophysical Survey of Slovenia, Ljubljana, Slovenia ;Zupancic, P.; Geophysical Survey of Slovenia, Ljubljana, Slovenia; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; The Adriatic region was chosen as one of the test areas in the GSHAP program and, consequently, its seismic hazard was computed. The standard hazard map chosen by GSHAP represents PGA with a 475-year return period. Some other parameters, as the spectral acceleration and the uniform hazard response spectra for the main Adriatic towns, have been computed for a better representation of the regional hazard. The most hazardous area remains identified in the Cephalonia zone, where strong earthquakes frequently occur. The Southern Apennines are characterised by a slightly lower hazard, while the Adriatic Sea itself, the Poplain and the Apulian peninsula are almost aseismic.344 717 - PublicationOpen AccessThe reliability of reported depths of some earthquake sequences in Northwestern Greece (Epirus and Corfu Island) and the geodynamic situation of the area(1996-12)
; ;Muço, B.; Seismological Institute, Tirana, AlbaniaThe study of the earthquakes of the rectangle with coordinates 39°-40°N 19°-21°E is very important for a better understanding of the geodynamics of this area. In and near this zone, the subduction of the Aegean arc stops, and northward, going to the Albanian coast, the confrontation between the Adria microplate and the Albanian orogen is probably of collisional type. In this approach based on records of Greek seismological stations situated in this area as well as southern stations of the Albanian Seismological Network (ASN), the depth of the earthquakes of some sequences that occurred recently in this zone is carefully investigated. Some records of Southern Albanian seismological stations resulting from earthquakes with the same epicentral zone but reported with different depth are compared. The importance of detailed studies of this zone is stressed to shed light on the geodynamics of a key segment of the northwestern end of the Aegean arc.159 181