Large‐displacement, hydrothermal frictional properties of DFDP‐1 fault rocks, Alpine Fault, New Zealand: Implications for deep rupture propagation

The Alpine Fault, New Zealand, is a major plate‐bounding fault that accommodates 65–75% of the total relative motion between the Australian and Pacific plates. Here we present data on the hydrothermal frictional properties of Alpine Fault rocks that surround the principal slip zones (PSZ) of the Alp...

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Detalles Bibliográficos
Autores principales: Niemeijer, A. R., Boulton, C., Toy, V. G., Townend, J., Sutherland, R.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2016
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4994769/
https://www.ncbi.nlm.nih.gov/pubmed/27610290
http://dx.doi.org/10.1002/2015JB012593

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4994769/
https://www.ncbi.nlm.nih.gov/pubmed/27610290
http://dx.doi.org/10.1002/2015JB012593

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