Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Simone, Masoch"'
Autor:
Simone Masoch, Michele Fondriest, Rodrigo Gomila, Giorgio Pennacchioni, José Cembrano, Giulio Di Toro
Faults can act as conduits for the migration of hydrothermal fluids in the crust, affecting its mechanical behaviour and possibly leading to earthquake swarm activity. To date, there are still few constraints from the geological record on how fault-v
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::52cdf8d017954f893c18cfb8cf5179d6
https://doi.org/10.5194/egusphere-egu23-531
https://doi.org/10.5194/egusphere-egu23-531
Autor:
Simone Masoch, Michele Fondriest, Rodrigo Gomila, Erik Jensen, Giulia Magnarini, Javier Espinosa, Karin Hofer, Tom Mitchell, José Cembrano, Giorgio Pennacchioni, Giulio Di Toro
Fault zone architecture controls, for instance, the nucleation, propagation and arrest of individual seismic ruptures, the moment magnitude of the mainshocks and the evolution in space and time of foreshock and aftershock seismic sequences. Neverthel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::03c7b666453cd0944bb9db590c213e53
https://doi.org/10.5194/egusphere-egu22-1926
https://doi.org/10.5194/egusphere-egu22-1926
Autor:
Simone Masoch, Michele Fondriest, Rodrigo Gomila, Erik Jensen, Thomas M. Mitchell, José Cembrano, Giorgio Pennacchioni, Giulio Di Toro
Publikováno v:
Journal of Structural Geology. 165:104745
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9b22d24ee97d66ea793954b8724069e7
https://doi.org/10.1016/j.jsg.2022.104745
https://doi.org/10.1016/j.jsg.2022.104745
Autor:
Thomas M. Mitchell, Giulio Di Toro, Erik Jensen, Simone Masoch, Giorgio Pennacchioni, José Cembrano, Rodrigo Gomila, Michele Fondriest
Publikováno v:
Tectonics
Tectonics, 2021, 40, pp.1730-1746. ⟨10.1029/2021TC006818⟩
Tectonics, 2021, 40, pp.1730-1746. ⟨10.1029/2021TC006818⟩
How major crustal‐scale seismogenic faults nucleate and evolve in crystalline basements represents a long‐standing, but poorly understood, issue in structural geology and fault mechanics. Here, we address the spatio‐temporal evolution of the Bo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d2968a8560b7b426732c23fec3681050
https://doi.org/10.1002/essoar.10506525.1
https://doi.org/10.1002/essoar.10506525.1
Autor:
José Cembrano, Silvia Mittempergher, Elena Spagnuolo, Rodrigo Gomila, Thomas M. Mitchell, Andrea Bistacchi, Simone Masoch, Michele Fondriest, G. Di Toro, Daniel R. Faulkner, G. Magnarini, Erik Jensen
Publikováno v:
Geochemistry, Geophysics, Geosystems
Geochemistry, Geophysics, Geosystems, 2021, 22, p. 263-281. ⟨10.1029/2021GC009743⟩
Geochemistry, Geophysics, Geosystems : G(3)
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
Geochemistry, Geophysics, Geosystems, 2021, 22, p. 263-281. ⟨10.1029/2021GC009743⟩
Geochemistry, Geophysics, Geosystems : G(3)
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
Tectonic pseudotachylytes are thought to be unique to certain water‐deficient seismogenic environments and their presence is considered to be rare in the geological record. Here, we present field and experimental evidence that frictional melting ca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::512304460b3e16b5f5d1c87fe2bc0607
https://hal-insu.archives-ouvertes.fr/insu-03594400/document
https://hal-insu.archives-ouvertes.fr/insu-03594400/document
Autor:
Rodrigo Gomila, Erik Jensen, Michele Fondriest, Giulio Di Toro, Thomas Mitchell, Andrea Bistacchi, Carlo Sommacampagna, Simone Masoch, Giulia Magnarini, José Cembrano
The geometry of fault zones (e.g. fault surface roughness, fault rock distribution, network of secondary faults andfractures) is one of the main factors controlling earthquake nucleation, rupture speed and length of main shocks,foreshock and aftersho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1299::a0d2914f86ad4178c50554b4f2fb7e0d
http://hdl.handle.net/10281/299857
http://hdl.handle.net/10281/299857
Autor:
Giulio Di Toro, Michele Fondriest, Thomas Mitchell, Rodrigo Gomila, Erik Jensen, CarloSommacampagna, Simone Masoch, Andrea Bistacchi, Giulia Magnarini, Dan Faulkner, JoséCembrano, Silvia Mittempergher
Pseudotachylytes (solidified friction melts produced during seismic slip) are currently considered one of the veryfew geological markers of seismic faulting in exhumed faults. Pseudotachylytes are thought to be rare in thegeological record because th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1299::fc32c7e82329ef213e81294b1fc87b2b
http://hdl.handle.net/10281/299855
http://hdl.handle.net/10281/299855
Autor:
José Cembrano, Andrea Bistacchi, Michele Fondriest, Simone Masoch, Thomas M. Mitchell, Elena Spagnuolo, Silvia Mittempergher, Erik Jensen, Rodrigo Gomila, Giulio Di Toro, G. Magnarini, Daniel R. Faulkner
Pseudotachylytes (solidified friction melts produced during seismic slip) are considered to be rare in the geological record because they should be typical of particular seismogenic environments characterized by water-deficient cohesive rocks. Here w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::559959a9ade01b980a6c16b8d54e6f8e
http://hdl.handle.net/10281/299861
http://hdl.handle.net/10281/299861
Publikováno v:
Journal of Structural Geology. 129:103889
Few fault rocks are known to be associated undoubtedly with seismic faulting. Here, we investigated the formation mechanism of cockade breccias found in transtensional faults cutting marbles and quartzites from the Col de Teghime area (Alpine Corsica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5dab08df46df925dcd4de488d9bb8dad
https://doi.org/10.1016/j.jsg.2019.103889
https://doi.org/10.1016/j.jsg.2019.103889