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Is complex fault zone behaviour a reflection of rheological heterogeneity?
Fault slip speeds range from steady plate boundary creep through to earthquake slip. Geological descriptions of faults range from localized displacement on one or more discrete planes, through to distributed shearing flow in tabular zones of finite thickness, indicating a large range of possible str...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
The Royal Society Publishing
2021
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7898124/ https://www.ncbi.nlm.nih.gov/pubmed/33517872 http://dx.doi.org/10.1098/rsta.2019.0421 |