Zobrazeno 1 - 10
of 79
pro vyhledávání: '"high‐velocity friction"'
Publikováno v:
Journal of Geophysical Research: Solid Earth, 127(11)
Earthquake simulation and hazard prediction are strongly hampered by insufficient physical knowledge of the constitutive behavior of faults. Laboratory studies of carbonate fault friction suggest that seismogenic rupture on faults in carbonate terrai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1d928cb0baedb6de46e5d08050d89806
https://doi.org/10.1029/2022jb024530
https://doi.org/10.1029/2022jb024530
Akademický článek
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Akademický článek
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Publikováno v:
Journal of Geophysical Research: Solid Earth, 126(3), 1
Journal of Geophysical Research. Solid Earth
Journal of Geophysical Research. Solid Earth
Laboratory studies suggest that seismogenic rupture on faults in carbonate terrains can be explained by a transition from high friction, at low sliding velocities (V), to low friction due to rapid dynamic weakening as seismic slip velocities are appr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e9ecef5c5027da320d2e8c311b69091a
https://dspace.library.uu.nl/handle/1874/412595
https://dspace.library.uu.nl/handle/1874/412595
Laboratory studies suggest that seismogenic rupture on faults in carbonate terrains can be explained by a transition from high friction, at low sliding velocities (V), to low friction due to rapid dynamic weakening as seismic slip velocities are appr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::68e2c489410006c2d39e7a5d049ef945
https://doi.org/10.1002/essoar.10504397.1
https://doi.org/10.1002/essoar.10504397.1
Autor:
Giulio Di Toro, H. S. Rabinowitz, Elena Spagnuolo, Heather M. Savage, Stefano Aretusini, Pratigya J. Polissar
Publikováno v:
Earth and Planetary Science Letters. 502:253-261
Evidence of temperature rise is useful for identifying where within a fault zone earthquake slip has occurred, as well as some attributes of the earthquake such as energy output. Biomarker thermal maturity can elucidate structures within a fault zone
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cefc9b8e8aa7e91e784ced16dd805bd0
https://doi.org/10.1016/j.epsl.2018.08.038
https://doi.org/10.1016/j.epsl.2018.08.038
Akademický článek
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Autor:
Aretusini, S., Plümper, O., Spagnuolo, E., Di Toro, G., Structural geology and EM, Structural geology & tectonics
Publikováno v:
Journal of Geophysical Research. Solid Earth
Journal of Geophysical Research: Solid Earth, 124(7), 6589
Journal of Geophysical Research: Solid Earth, 124(7), 6589
Smectite clays are the main constituent of slipping zones found in subduction zone faults at shallow depth (e.g.
Key Points Nanofoliations develop at subseismic to seismic slip rates in partly water saturated smectite fault gougesNanofoliations
Key Points Nanofoliations develop at subseismic to seismic slip rates in partly water saturated smectite fault gougesNanofoliations
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::548b0c33753c2d6b4ad6f1de855e3036
http://hdl.handle.net/11577/3308706
http://hdl.handle.net/11577/3308706
Publikováno v:
Rutter, E 2019, ' Water Availability and Deformation Processes inSmectite-Rich Gouges During Seismic Slip ', Journal of Geophysical Research: Solid Earth . https://doi.org/10.1029/2019JB018229
Smectite clays occur in subduction zone fault cores at shallow depth (approximately 1 km;e.g., Japan Trench) and landslide décollements (e.g., Vajont, Italy, 1963). The availability of porefluidsaffects the likelihood that seismic slip propagates fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6e3b6132b560ad0c0a9a9407fed11b4d
http://hdl.handle.net/11577/3330991
http://hdl.handle.net/11577/3330991
Flash Heating and Local Fluid Pressurization Lead to Rapid Weakening in Water-Saturated Fault Gouges
Autor:
Yao, Lu, Ma, Shengli, Chen, Jianye, Shimamoto, Toshihiko, He, Honglin, Experimental rock deformation
Publikováno v:
Journal of Geophysical Research: Solid Earth, 123(10), 9084. Wiley
Coseismic fault displacement is quite large at shallow depths in some earthquakes, and it implies that fault gouges and sediments have extremely low dynamic friction during seismic slip. However, the dynamic weakening mechanisms of gouges under wet c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9bc0c1f3375b36a077fdef274e31f6b8
https://dspace.library.uu.nl/handle/1874/374370
https://dspace.library.uu.nl/handle/1874/374370