Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Giovanni Diaferia"'
Autor:
Luca De Siena, Fabrizio Magrini, Nicolas Riel, Giovanni Diaferia, Francesca Forni, Boris J. P. Kaus
The crustal feeding systems under volcanoes like Toba caldera in Sumatra remain largely unknown due to the lack of existing seismic arrays and consistent effort to apply advanced imaging techniques. Even if they were obtained, the interpretation of s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e668e2bad6c520fd3993e59184311075
https://doi.org/10.5194/egusphere-egu23-4328
https://doi.org/10.5194/egusphere-egu23-4328
Autor:
Luisa Valoroso, Spina Cianetti, Pasquale De Gori, Giovanni Diaferia, Carlo Giunchi, Luigi Improta, Davide Piccinini, Luciano Zuccarello, Rocco Cogliano, Antonio Fodarella, Felice Minichiello, Stefania Pucillo, Francesca Di Luccio
The role of fluids in the preparatory phase of major earthquakes and in the evolution of aftershocks and swarms in space and time is well-documented. In particular, numerous studies evidence the primary role that mantle-derived fluids play in the gen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7aa132b6c614c4a15c613572b4546e27
https://doi.org/10.5194/egusphere-egu23-9565
https://doi.org/10.5194/egusphere-egu23-9565
Autor:
Matthew Agius, Fabrizio Magrini, Giovanni Diaferia, Emanuel Kastle, Fabio Cammarano, Claudio Faccenna, Francesca Funiciello, Mark van der Meijde
The evolution of the Sicily Channel Rift Zone (SCRZ), located south of the Central Mediterranean, is thought to accommodate the regional tectonic stresses of the Calabrian subduction system. It is unclear whether the rifting of the SCRZ is passive fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7a3b759410ff74e34e7d4d4d28f9a035
https://doi.org/10.5194/egusphere-egu22-4870
https://doi.org/10.5194/egusphere-egu22-4870
Improving the capability of seismic networks to detect small-magnitude seismicity, commonly near or below the detectability threshold, is the prerequisite to characterize the seismotectonics of an area in terms of fault geometry, kinematics and mecha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2c56e4f7107f6dcfef9a6253d900a548
https://doi.org/10.5194/egusphere-egu22-2007
https://doi.org/10.5194/egusphere-egu22-2007
Autor:
Fabrizio Magrini, Giovanni Diaferia, Amr El‐Sharkawy, Fabio Cammarano, Mark van der Meijde, Thomas Meier, Lapo Boschi
Publikováno v:
Journal of Geophysical Research: Solid Earth, 127(3):e2021JB023267. Wiley-Blackwell
The complex tectonic setting of the central-western Mediterranean has interested geoscientists for decades, but its geodynamic evolution remains a matter of debate. We rely on 807 seismometers from southern Europe and northern Africa to measure Rayle
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::72f9d80e8e0166fa6b09255beb9b2624
http://hdl.handle.net/11577/3443777
http://hdl.handle.net/11577/3443777
Autor:
Claudio Faccenna, Mark van der Meijde, Giovanni Diaferia, Matthew Agius, Fabrizio Magrini, Emanuel Kästle, Fabio Cammarano, Francesca Funiciello
Publikováno v:
EGU General Assembly 2021: Engage-Discover-Inspire
ISSUE=679;TITLE=EGU General Assembly 2021
ISSUE=679;TITLE=EGU General Assembly 2021
The Central Mediterranean, the area encompassing Italy, Sardinia, Tunisia and Libya, is characterised by multiple tectonic processes (plate convergence, subduction, and backarc extension). The evolution and interaction of the plate margins within thi
The dynamics of crustal extension and the crust-mantle interaction in the Central-Western Mediterranean and Italian peninsula (i.e. Liguro-Provençal and Tyrrhenian Basin), and plate convergence (i.e. Alpine and Apennines chains) are key for the unde
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::137ffb37951b7781216a947b5d12a18d
https://doi.org/10.5194/egusphere-egu21-15238
https://doi.org/10.5194/egusphere-egu21-15238
The shear-wave velocities structure at depth can be unraveled from ambient noise (AN) as well as from earthquake-generated (EQ) surface waves. While the first approach mostly provides information at crustal scale, earthquake-based surface waves sense
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3fd375ff18dd18f3ce57ed9fb8019835
https://doi.org/10.5194/egusphere-egu2020-7179
https://doi.org/10.5194/egusphere-egu2020-7179
Autor:
Mark van der Meijde, I. Fadel, Fabio Cammarano, Fabrizio Magrini, Lapo Boschi, Giovanni Diaferia
Publikováno v:
Geophysical journal international, 220(3), 2119-2130. Wiley-Blackwell
SUMMARY Rayleigh-wave dispersion curves from both ambient noise and teleseismic events allow us to provide the first high-resolution 3-D shear wave velocity (VS) model of the crust and upper mantle below the Sardinia–Corsica microplate, an importan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1df285592bd1399da05ea7ce1bf9690d
https://research.utwente.nl/en/publications/8e6d193a-f3e2-47ac-8898-527dc37d7342
https://research.utwente.nl/en/publications/8e6d193a-f3e2-47ac-8898-527dc37d7342
Autor:
Fabio Cammarano, Giovanni Diaferia
Publikováno v:
Tectonics. 36:3192-3208