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Heating, weakening and shear localization in earthquake rupture
Field and borehole observations of active earthquake fault zones show that shear is often localized to principal deforming zones of order 0.1–10 mm width. This paper addresses how frictional heating in rapid slip weakens faults dramatically, relative to their static frictional strength, and promotes...
Gorde:
| Argitaratua izan da: | Philos Trans A Math Phys Eng Sci |
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| Egile nagusia: | |
| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
The Royal Society Publishing
2017
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| Gaiak: | |
| Sarrera elektronikoa: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5580449/ https://ncbi.nlm.nih.gov/pubmed/28827427 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rsta.2016.0015 |
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