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Revealing the cluster of slow transients behind a large slow slip event

Capable of reaching similar magnitudes to large megathrust earthquakes [M(w) (moment magnitude) > 7], slow slip events play a major role in accommodating tectonic motion on plate boundaries through predominantly aseismic rupture. We demonstrate here that large slow slip events are a cluster of sh...

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Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Cyhoeddwyd yn:Sci Adv
Prif Awduron: Frank, William B., Rousset, Baptiste, Lasserre, Cécile, Campillo, Michel
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: American Association for the Advancement of Science 2018
Pynciau:
Mynediad Ar-lein:https://ncbi.nlm.nih.gov/pmc/articles/PMC5976274/
https://ncbi.nlm.nih.gov/pubmed/29854951
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aat0661
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