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Fast-moving dislocations trigger flash weakening in carbonate-bearing faults during earthquakes
Rupture fronts can cause fault displacement, reaching speeds up to several ms(−1) within a few milliseconds, at any distance away from the earthquake nucleation area. In the case of silicate-bearing rocks the abrupt slip acceleration results in melting at asperity contacts causing a large reduction...
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| Pubblicato in: | Sci Rep |
|---|---|
| Autori principali: | , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Nature Publishing Group
2015
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4639853/ https://ncbi.nlm.nih.gov/pubmed/26552964 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep16112 |
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