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Faulting of Rocks in a Three-Dimensional Stress Field by Micro-Anticracks
Nucleation and propagation of a shear fault is known to be the result of interaction and coalescence of many microcracks. Yet the character and rate of the microcracks' interactions, and their dependence on the three-dimensional stress state are poorly understood. Here we investigate formation...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group
2014
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4034368/ https://www.ncbi.nlm.nih.gov/pubmed/24862447 http://dx.doi.org/10.1038/srep05011 |