Bifurcations at the stability transition of earthquake faulting

Tectonic faults typically break in a single rupture mode within the range of styles from slow slip to dynamic earthquake failure. However, in increasingly well‐documented instances, the same fault segment fails in both slow and fast modes within a short period, as in the sequences that culminated in...

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Bibliographic Details
Main Authors: Mele Veedu, Deepa, Giorgetti, Carolina, Scuderi, Marco, Barbot, Sylvain, Marone, Chris, Collettini, Cristiano
Other Authors: Earth Observatory of Singapore
Format: Article
Language:English
Published: 2021
Subjects:
Online Access:https://hdl.handle.net/10356/146197
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Institution: Nanyang Technological University
Language: English
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