Nanometric flow and earthquake instability
Extremely fine-grained fault rocks are intrinsically weak and behave as fluids even at low temperatures and fast deformation rates. Local production of fine-grained material during fault movement can lead to an earthquake instability.
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| Autores principales: | , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2021
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/9e9a8646939945ca8bd2b82b9058e360 |
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