 |
Article dans une revue
The Transient and Intermittent Nature of Slow Slip
Abstract : To first order, faults are locked while stress builds up to a devastating earthquake. However, we know that faults also slip slowly. After decades of geophysical observation, slow slip is now recognized as part of a continuum of transient deformation ranging from the dynamic propagation of seismic rupture to aseismic events over a wide range of durations and sizes. A growing body of evidence suggests that large-scale slow slip events can be decomposed into a multitude of smaller, temporally clustered events. Slow slip is more frequent and more dynamic than is suggested by conceptual models of rate-strengthening, stable slip.
https://hal-ens.archives-ouvertes.fr/hal-02944816
Contributeur : Romain Jolivet <>
Soumis le : vendredi 16 avril 2021 - 09:27:36
Dernière modification le : vendredi 2 juillet 2021 - 10:46:03
Archivage à long terme le : : samedi 17 juillet 2021 - 18:17:00
Contributeur : Romain Jolivet <>
Soumis le : vendredi 16 avril 2021 - 09:27:36
Dernière modification le : vendredi 2 juillet 2021 - 10:46:03
Archivage à long terme le : : samedi 17 juillet 2021 - 18:17:00
Fichier
2019AV000126.pdf
Publication financée par une institution
Licence
Distributed under a Creative Commons Paternité - Pas de modifications 4.0 International License
