Induced seismicity provides insight into why earthquake ruptures stop.

Citation data:

Science advances, ISSN: 2375-2548, Vol: 3, Issue: 12, Page: eaap7528

Publication Year:
2017
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Repository URL:
http://hdl.handle.net/10754/626443
PMID:
29291250
DOI:
10.1126/sciadv.aap7528
Author(s):
Galis, Martin; Ampuero, Jean Paul; Mai, Paul Martin; Cappa, Frédéric
Publisher(s):
American Association for the Advancement of Science (AAAS)
Tags:
Multidisciplinary
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article description
Injection-induced earthquakes pose a serious seismic hazard but also offer an opportunity to gain insight into earthquake physics. Currently used models relating the maximum magnitude of injection-induced earthquakes to injection parameters do not incorporate rupture physics. We develop theoretical estimates, validated by simulations, of the size of ruptures induced by localized pore-pressure perturbations and propagating on prestressed faults. Our model accounts for ruptures growing beyond the perturbed area and distinguishes self-arrested from runaway ruptures. We develop a theoretical scaling relation between the largest magnitude of self-arrested earthquakes and the injected volume and find it consistent with observed maximum magnitudes of injection-induced earthquakes over a broad range of injected volumes, suggesting that, although runaway ruptures are possible, most injection-induced events so far have been self-arrested ruptures.