Nucleation of Stick‐Slip Instability Within a Large‐Scale Experimental Fault: Effects of Stress Heterogeneities Due to Loading and Gouge Layer Compaction

Geodetic observations and large‐scale laboratory experiments show that seismic instability is preceded by slow slip within a finite nucleation zone. In laboratory experiments rupture nucleation is studied mostly using bare (rock) interfaces, whereas upper crustal faults are typically filled with gou...

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Detalles Bibliográficos
Autores principales: Buijze, L., Guo, Y., Niemeijer, A. R., Ma, S., Spiers, C. J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2020
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7507769/
https://www.ncbi.nlm.nih.gov/pubmed/32999804
http://dx.doi.org/10.1029/2019JB018429

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7507769/
https://www.ncbi.nlm.nih.gov/pubmed/32999804
http://dx.doi.org/10.1029/2019JB018429

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