Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Valère, Lambert"'
Autor:
Valère Lambert
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 11, Pp n/a-n/a (2024)
Abstract Fault regions inferred to be slowly slipping are interpreted to accommodate much of tectonic plate motion aseismically and potentially serve as barriers to earthquake rupture. Here, we build on prior work using simulations of earthquake sequ
Externí odkaz:
https://doaj.org/article/55f3ecacce4844c8b1ee2ccb347fc592
Autor:
Brittany A. Erickson, Junle Jiang, Valère Lambert, Sylvain D. Barbot, Mohamed Abdelmeguid, Martin Almquist, Jean-Paul Ampuero, Ryosuke Ando, Camilla Cattania, Alexandre Chen, Luca Dal Zilio, Shuai Deng, Eric M. Dunham, Ahmed E. Elbanna, Alice-Agnes Gabriel, Tobias W. Harvey, Yihe Huang, Yoshihiro Kaneko, Jeremy E. Kozdon, Nadia Lapusta, Duo Li, Meng Li, Chao Liang, Yajing Liu, So Ozawa, Andrea Perez-Silva, Casper Pranger, Paul Segall, Yudong Sun, Prithvi Thakur, Carsten Uphoff, Ylona van Dinther, Yuyun Yang
Publikováno v:
Bulletin of the Seismological Society of America, 113 (2)
Numerical modeling of earthquake dynamics and derived insight for seismic hazard relies on credible, reproducible model results. The sequences of earthquakes and aseismic slip (SEAS) initiative has set out to facilitate community code comparisons, an
In the framework of empirically-derived rate- and state- friction (RSF) laws, friction constitutive parameters a, b, and Dc (and further sets of state parameters) are obtained from inverse modelling of laboratory data on the assumption that steady-st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::36a0cdcd3e1263a2142772bc486cba01
https://doi.org/10.5194/egusphere-egu23-15563
https://doi.org/10.5194/egusphere-egu23-15563
Autor:
Brittany A. Erickson, Junle Jiang, Casper Pranger, Meng Li, Benchun Duan, Alice-Agnes Gabriel, So Ozawa, Nadia Lapusta, Eric M. Dunham, Sylvain Barbot, Jean-Paul Ampuero, Ryosuke Ando, Ylona van Dinther, Yajing Liu, Duo Li, Luca Dal Zilio, Valère Lambert, Dunyu Liu, Camilla Cattania
Dynamic modeling of sequences of earthquakes and aseismic slip (SEAS) provides a self-consistent, physics-based framework to connect, interpret, and predict diverse geophysical observations across ...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::157b2b774f56fc0f50e77389ff05a7f1
https://doi.org/10.1002/essoar.10508582.2
https://doi.org/10.1002/essoar.10508582.2
Heterogeneity of fault zones is seen at all scales in nature. It may manifest itself in terms of the variability of material property distribution over the fault, of stress heterogeneity brought about by the history of previous earthquake ruptures, a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4172f1c1bc939710ba332cfee101e271
https://doi.org/10.5194/egusphere-egu21-8058
https://doi.org/10.5194/egusphere-egu21-8058
Autor:
Victor C. Tsai, Valère Lambert
Over recent decades, it has become clear that the extraction of fluids from underground reservoirs can be linked to seismicity and aseismic deformation around producing fields. Using a simple model with uniform fluid extraction from a reservoir, Sega
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fd12334f366416ec548bede15b4fe969
https://resolver.caltech.edu/CaltechAUTHORS:20200813-074456541
https://resolver.caltech.edu/CaltechAUTHORS:20200813-074456541
Stress drops, inferred to be magnitude‐invariant, are a key characteristic used to describe natural earthquakes. Theoretical studies and laboratory experiments indicate that enhanced dynamic weakening, such as thermal pressurization of pore fluids,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b08938e7959aa820243399db93984656
https://resolver.caltech.edu/CaltechAUTHORS:20200306-132842975
https://resolver.caltech.edu/CaltechAUTHORS:20200306-132842975
Publikováno v:
Bulletin of the Seismological Society of America. 107:821-855
We present a suite of analytical and semianalytical solutions for the displacements, strains, and stress due to distributed anelastic deformation of finite strain volumes in a half‐space for cuboid sources. We provide the solutions in the cases of
Publikováno v:
Nature. 591(7849)
Observations suggest that mature faults host large earthquakes at much lower levels of stress than their expected static strength1–11. Potential explanations are that the faults are quasi-statically strong but experience considerable weakening duri