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Stable isotopes show that earthquakes enhance permeability and release water from mountains
Hydrogeological properties can change in response to large crustal earthquakes. In particular, permeability can increase leading to coseismic changes in groundwater level and flow. These processes, however, have not been well-characterized at regional scales because of the lack of datasets to descri...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2020
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7265347/ https://www.ncbi.nlm.nih.gov/pubmed/32488089 http://dx.doi.org/10.1038/s41467-020-16604-y |