Zobrazeno 1 - 10
of 90
pro vyhledávání: '"Francesca Funiciello"'
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
Subduction megathrusts host the Earth’s greatest earthquakes as the 1960 Valdivia (Mw 9.5, Chile), the largest earthquake instrumentally recorded, and the recent 2004 Sumatra-Andaman (Mw 9.2, Indonesia), 2010 Maule (Mw 8.8, Chile), and 2011 Tohoku-
Externí odkaz:
https://doaj.org/article/319bbf1790b544dc87272c184838fdbd
Autor:
Mireia Peral, Jonas Ruh, Sergio Zlotnik, Francesca Funiciello, Manel Fernàndez, Jaume Vergés, Taras Gerya
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 21, Iss 6, Pp n/a-n/a (2020)
Abstract In this work we study the dynamics of double subduction systems with opposite polarity in adjacent segments. A combined approach of numerical and analog experiments allows us to compare results and exploit the strengths of both methodologies
Externí odkaz:
https://doaj.org/article/a74e5d0b0196405bb2d4e40277f89366
Autor:
Elenora vanRijsingen, Serge Lallemand, Michel Peyret, Diane Arcay, Arnauld Heuret, Francesca Funiciello, Fabio Corbi
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 19, Iss 8, Pp 2342-2370 (2018)
Abstract The role of seafloor roughness on the seismogenic behavior of subduction zones has been increasingly addressed over the past years, although their exact relationship remains unclear. Do subducting features like seamounts, fracture zones, or
Externí odkaz:
https://doaj.org/article/c189cf8e589f4d8d9d7c5a9ffba951d0
Autor:
Irene Menichelli, Fabio Corbi, Silvia Brizzi, Elenora van Rijsingen, Francesca Funiciello, Serge Lallemand
It has been widely recognized that the presence of seamounts can profoundly affect megathrust seismicity. With their outstanding topography, seamounts can tune interplate stress and favor the development of a fracture network in the overriding plate.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7815e1a4577afb6f34f141a192f36cbc
https://doi.org/10.5194/egusphere-egu23-4981
https://doi.org/10.5194/egusphere-egu23-4981
Autor:
Fabio Corbi, Giacomo Mastella, Elisa Tinti, Matthias Rosenau, Laura Sandri, Silvio Pardo, Francesca Funiciello
Accurate assessment of rate and state friction parameters is essential for producing realistic rupture scenarios and, in turn, for seismic hazard analysis. Those parameters can be directly measured in the laboratory, with experimental apparati that r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::99b3bb98f35d0c0b47d6314fb8ffeba4
https://doi.org/10.5194/egusphere-egu23-5411
https://doi.org/10.5194/egusphere-egu23-5411
Recent observations from Global Navigation Satellite Systems (GNSS) displacement time-series have demonstrated that the motion of tectonic plates is ubiquitously not steady-state. GNSS displacement time-series can be described as the sum of expected
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b140e50c7a011141ed896e3475c0948d
https://doi.org/10.5194/egusphere-egu23-5560
https://doi.org/10.5194/egusphere-egu23-5560
Autor:
Riccardo Reitano, Claudio Faccenna, Francesca Funiciello, Fabio Corbi, Riccardo Lanari, Romano Clementucci
The presence of a strong interaction between tectonic deformation and surface processes is widely recognized. Still, the nature of this interaction is difficult to unravel and quantify. In the last decades, analogue landscape evolution models have be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d896629982fe155455145537ec35016c
https://doi.org/10.5194/egusphere-egu22-9524
https://doi.org/10.5194/egusphere-egu22-9524
Autor:
Francesca FUNICIELLO
The use of experimental tectonics (also known as analogue-, laboratory, or physical modelling) to study tectonic processes is not a novelty in Earth Science. Following Sir James Hall’s pioneer work (1815), many modellers squeezed, stretched, pushed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4b1f0a1abc8d8de5227b5cb9f4969a1b
https://doi.org/10.5194/egusphere-egu22-13304
https://doi.org/10.5194/egusphere-egu22-13304
Autor:
Matthias Rosenau, Fabio Corbi, Nadaya Cubas, Francesca Funiciello, Ehsan Kosari, Bertrand Maillot, Giacomo Mastella, Onno Oncken, Michael Rudolf, Pauline Souloumiac, Sarah Visage
Tectonic faults display a range of slip behaviours including continuous and episodic slip covering rates of more than 10 orders of magnitude. To gain insight into the slip behaviour of brittle faults, we performed laboratory stick-slip experiments at
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78e9df8cae6b51e7b9c97da321de9506
https://doi.org/10.5194/egusphere-egu22-4533
https://doi.org/10.5194/egusphere-egu22-4533
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