Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Antonio Scaltrito"'
Autor:
Salvatore Alparone, Vincenza Maiolino, Antonino Mostaccio, Antonio Scaltrito, Andrea Ursino, Graziella Barberi, Salvatore D’Amico, Giuseppe Di Grazia, Elisabetta Giampiccolo, Carla Musumeci, Luciano Scarfì, Luciano Zuccarello
Publikováno v:
Annals of Geophysics, Vol 58, Iss 4 (2015)
Instrumental seismic catalogues are an essential tool for the zonation of the territory and the production of seismic hazard maps. They are also a valuable instrument for detailed seismological studies regarding active volcanoes and, above all, for i
Externí odkaz:
https://doaj.org/article/ae35f898e92f43c69c91de72563e7aec
Autor:
Elisabetta Giampiccolo, Luciano Scarfì, Vincenza Maiolino, Salvatore Alparone, Graziella Barberi, Carla Musumeci, A. Mostaccio, A. Ursino, Tiziana Tuvè, Antonio Scaltrito
Publikováno v:
Terra Nova. 32:334-344
Autor:
Salvatore Gambino, Antonio Scaltrito
Publikováno v:
Journal of Volcanology and Geothermal Research. 350:1-6
The seismicity of Stromboli comprises explosion-quakes, volcanic tremor and volcano-tectonic (VT) events. We applied the double-difference approach of Waldhauser and Ellsworth (2000) on 42 VT events recorded during 2005–2016 in order to improve the
Publikováno v:
Advances in Geosciences, Vol 36, Pp 39-47 (2013)
Seismology and geodesy are generally seen as the most reliable diagnostic tools for monitoring highly active or erupting volcanoes, like Mt. Etna. From the early 1980's, seismic activity was monitored at Mt. Etna by a permanent seismic network, progr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3c6d571593cc11539f1c35db8c98ad03
https://adgeo.copernicus.org/articles/36/39/2013/
https://adgeo.copernicus.org/articles/36/39/2013/
Autor:
Salvatore Gambino, Giuseppe Tortorici, Mimmo Palano, Gino Romagnoli, Francesco Pavano, Stefano Catalano, Antonio Scaltrito, Laura Cammarata
Between June 2011 and September 2013, the Nebrodi Mountains region was affected by a seismic swarm consisting of > 2700 events with local magnitude 1.3 ≤ ML ≤ 4.6 and located in the 5–9 km depth interval. The seismic swarm defines a seismogenet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3b71c7eff6a5974c24ad7a5169efe3fd
http://hdl.handle.net/20.500.11769/314414
http://hdl.handle.net/20.500.11769/314414
WOS: 000403135300003
During the first days of December 2015, there were four paroxysmal events at the "Voragine" crater on Mount Etna, which were among the most violent observed during the last two decades. A few days after the "Voragine" paroxy
During the first days of December 2015, there were four paroxysmal events at the "Voragine" crater on Mount Etna, which were among the most violent observed during the last two decades. A few days after the "Voragine" paroxy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c2592f8986fdb1d05b1b8caec63baf0f
https://hdl.handle.net/20.500.12628/3477
https://hdl.handle.net/20.500.12628/3477
Publikováno v:
Tectonophysics. :108-115
To recognize possible spatial clusters and identify active seismogenic zones and structures in the Aeolian Archipelago, in the south of Italy, we analyzed the spatial pattern of seismicity between 1993 and 2010 in a selected area comprising Vulcano,
Publikováno v:
Physics of the Earth and Planetary Interiors. 177:65-78
The Messina Strait is the most important structural element interrupting the southernmost part of the Alpine-Apenninic orogenic belt, known as the Calabro-Peloritan Arc. It is being a narrow fan-shaped basin linking the Ionian Sea to the Tyrrhenian S
Publikováno v:
Journal of Volcanology and Geothermal Research. 178:795-806
The Peloritani Mts. (NE Sicily) are characterized by frequent seismicity. Between 1994 and 2006 more than 1000 earthquakes (1.0 ≤ ML ≤ 3.3) occurred, mostly as highly clustered swarms located at shallow depth near the villages of Castroreale and
Publikováno v:
Geophysical Journal International. 170:1151-1164
SUMMARY Accurate earthquake locations are of primary importance when studying the seismicity of a given area, they allow important inferences on the ongoing seismo-tectonics. Both, for standard, as well as for earthquake relative location techniques,