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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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| Vydáno v: | Sci Adv |
|---|---|
| Hlavní autoři: | , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
American Association for the Advancement of Science
2018
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| Témata: | |
| On-line přístup: | 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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