Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Jérôme Aubry"'
Autor:
Martin Colledge, Jérôme Aubry, Kristel Chanard, François Pétrélis, Clara Duverger, Laurent Bollinger, Alexandre Schubnel
Small transient stress perturbations are prone to trigger (micro)seismicity. In the Earth's crust, these stress perturbations can be caused by various sources such as the passage of seismic waves, tidal forcing, or hydrological seasonal loads. A bett
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15ce3dc97d4b067d00ae9a051901cf8b
https://doi.org/10.5194/egusphere-egu23-2833
https://doi.org/10.5194/egusphere-egu23-2833
We propose a numerical model of laboratory earthquake cycle inspired by a set of experiments performed on a triaxial apparatus on sawcut Carrara marble samples. The model couples two representations of rock matter: rock is essentially represented as
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15f33c630a3beab9cfa832abe45c0a92
https://doi.org/10.5194/egusphere-egu23-6517
https://doi.org/10.5194/egusphere-egu23-6517
Autor:
Martin Colledge, Jérôme Aubry, Kristel Chanard, François Pétrélis, Clara Duverger, Laurent Bollinger, Alexandre Schubnel
Publikováno v:
Journal of Geophysical Research : Solid Earth
Journal of Geophysical Research : Solid Earth, 2023, 128 (4), ⟨10.1029/2022JB025583⟩
Journal of Geophysical Research : Solid Earth, 2023, 128 (4), ⟨10.1029/2022JB025583⟩
International audience
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ec450f66da26f31d99b949a5f4b13b4a
https://hal.science/hal-04093180/document
https://hal.science/hal-04093180/document
Publikováno v:
Journal of Geophysical Research: Solid Earth. 128
Autor:
Martin Colledge, Kristel Chanard, Jérôme Aubry, François Pétrélis, Clara Duverger, Laurent Bollinger, Alexandre Schubnel
Small transient stress perturbations are prone to trigger (micro)seismicity. In the Earth's crust, these transient stress changes can be caused by various sources : passing of seismic waves, forcing by tides, hydrological load, and other seasonal cli
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1d92985760848a0cfc5529568919c019
https://doi.org/10.5194/egusphere-egu22-6034
https://doi.org/10.5194/egusphere-egu22-6034
In this communication, we present a novel numerical framework which consists in a direct coupling between a discrete micromechanical modelling of rock damaging processes and a continuous modelling of elastic deformation and acoustic waves. It include
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d48c44df5cb25c944b425b099c15d983
https://doi.org/10.5194/egusphere-egu21-1114
https://doi.org/10.5194/egusphere-egu21-1114
Publikováno v:
Journal of Geophysical Research: Solid Earth
Journal of Geophysical Research: Solid Earth, 2021, 126 (6), ⟨10.1029/2020JB021485⟩
Journal of Geophysical Research: Solid Earth, 2021, 126 (6), ⟨10.1029/2020JB021485⟩
Autor:
Alexandre Schubnel, Samson Marty, Damien Deldicque, Javier Escartín, Jérôme Aubry, Marine Page, Julien Gasc, Francois Passelegue
In the lithosphere, the transition from brittle to ductile deformation corresponds to a regime where brittle fracturing and plastic flow coexist, called the semi-brittle deformation zone. Within these different regimes, a large fault slip spectrum ha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aec1432fc9309f5f7dd910e923ca823d
https://doi.org/10.5194/egusphere-egu2020-4092
https://doi.org/10.5194/egusphere-egu2020-4092