Zobrazeno 1 - 8
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pro vyhledávání: '"Adinolfi G. M."'
Autor:
Adinolfi G. M., De Landro G., Picozzi M., Carotenuto F., Caruso A., Nazeri S., Colombelli S., Tarantino S., Muzellec T., Emolo A., Zollo A., Orefice A., Ulivieri B., Calcagni D., Piantanida M.
Publikováno v:
Frontiers in Earth Science. 11
A modern digital seismic network, with many stations optimally distributed on the earthquake causative seismic zone, enables detection of very low magnitude earthquakes and determination of their source parameters. It is essential to associate to suc
Akademický článek
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Akademický článek
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Publikováno v:
Journal of Seismology; Oct2020, Vol. 24 Issue 5, p979-989, 11p
Publikováno v:
IEEE Transactions on Geoscience and Remote Sensing. 60:1-10
With the aim to investigate the rupture complexity and the radiated wave field of 2017, Mw 3.9, Ischia earthquake, south-west of Naples (Italy), we used finite-fault modeling to invert the near-source (and searched for the best-fit kinematic rupture
Publikováno v:
Solid Earth, Vol 13, Pp 65-83 (2022)
Improving the knowledge of seismogenic faults requires the integration of geological, seismological, and geophysical information. Among several analyses, the definition of earthquake focal mechanisms plays an essential role in providing information a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::64d857a0443c58b62046abcf9b80b51c
https://doi.org/10.5194/se-2021-88
https://doi.org/10.5194/se-2021-88
Publikováno v:
Journal of Seismology
A coherence-based earthquake detection technique was applied to continuous (1 year) waveform data recorded along the Irpinia fault system (Southern Italy). The earthquake detection was performed using coherent P- and S-wave arrivals recorded by the d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5185af7fdf23d3690a4b29236efe4c99
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5002559
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5002559
Publikováno v:
Geophysical Journal International
SUMMARYMicroseismic monitoring is a primary tool for understanding and tracking the progress of mechanical processes occurring in active rock fracture systems. In geothermal or hydrocarbon fields or along seismogenic fault systems, the detection and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::82bb30feb4a8acc30e205e5b9fa7383d
https://hdl.handle.net/2318/1894834
https://hdl.handle.net/2318/1894834