Articles | Volume 33, issue 6
https://doi.org/10.5194/ejm-33-675-2021
https://doi.org/10.5194/ejm-33-675-2021
Research article
 | 
10 Nov 2021
Research article |  | 10 Nov 2021

New insights in the mechanisms of the reaction 3.65 Å phase  =  clinoenstatite + water down to nanoscales

Monika Koch-Müller, Oona Appelt, Bernd Wunder, and Richard Wirth

Viewed

Total article views: 1,170 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
789 319 62 1,170 110 60 113
  • HTML: 789
  • PDF: 319
  • XML: 62
  • Total: 1,170
  • Supplement: 110
  • BibTeX: 60
  • EndNote: 113
Views and downloads (calculated since 10 Nov 2021)
Cumulative views and downloads (calculated since 10 Nov 2021)

Viewed (geographical distribution)

Total article views: 1,152 (including HTML, PDF, and XML) Thereof 1,152 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 02 Dec 2025
Short summary
Dense hydrous magnesium silicates, like the 3.65 Å phase, are thought to cause deep earthquakes. We investigated the dehydration of the 3.65 Å phase at P and T. In both directions of the investigated simple reaction, additional metastable water-rich phases occur. The observed extreme reduction in grain size in the dehydration experiments might cause mechanical instabilities in the Earth’s mantle and, finally, induce earthquakes.
Share