Solid Earth
Solid Earth
SE
Articles | Volume 12, issue 1
Articles | Volume 12, issue 1
https://doi.org/10.5194/se-12-171-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/se-12-171-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 12, issue 1
Research article
 | 
25 Jan 2021
Research article |  | 25 Jan 2021

Effect of normal stress on the frictional behavior of brucite: application to slow earthquakes at the subduction plate interface in the mantle wedge

Hanaya Okuda, Ikuo Katayama, Hiroshi Sakuma, and Kenji Kawai

Viewed

Total article views: 2,612 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,939 614 59 2,612 134 57 53
  • HTML: 1,939
  • PDF: 614
  • XML: 59
  • Total: 2,612
  • Supplement: 134
  • BibTeX: 57
  • EndNote: 53
Views and downloads (calculated since 26 Aug 2020)
Cumulative views and downloads (calculated since 26 Aug 2020)

Viewed (geographical distribution)

Total article views: 2,612 (including HTML, PDF, and XML) Thereof 2,305 with geography defined and 307 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 02 May 2025
Download
Short summary
Serpentinite, generated by the hydration of ultramafic rocks, is thought to be related to slow earthquakes at the subduction plate interface in the mantle wedge. We conducted friction experiments on brucite, one of the components of serpentinite, and found that wet brucite exhibits low and unstable friction under low effective normal stress conditions. This result suggests that wet brucite may be key for slow earthquakes at the subduction plate interface in a hydrated mantle wedge.
Read more
Share
Special issue
Thermo-hydro-mechanical–chemical (THMC) processes in natural...