European Journal of Mineralogy
European Journal of Mineralogy
European Journal of Mineralogy
Articles | Volume 34, issue 2
Articles | Volume 34, issue 2
Eur. J. Mineral., 34, 201–213, 2022
https://doi.org/10.5194/ejm-34-201-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
Eur. J. Mineral., 34, 201–213, 2022
https://doi.org/10.5194/ejm-34-201-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 34, issue 2
Research article
31 Mar 2022
Research article | 31 Mar 2022

In situ reinvestigation of reaction phase A plus high-pressure clinoenstatite to forsterite plus water in the system MgO-SiO2-H2O (MSH)

Christian Lathe et al.

Viewed

Total article views: 210 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
155 49 6 210 21 3 5
  • HTML: 155
  • PDF: 49
  • XML: 6
  • Total: 210
  • Supplement: 21
  • BibTeX: 3
  • EndNote: 5
Views and downloads (calculated since 31 Mar 2022)
Cumulative views and downloads (calculated since 31 Mar 2022)

Viewed (geographical distribution)

Total article views: 193 (including HTML, PDF, and XML) Thereof 193 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 26 Jun 2022
Download
Short summary
The equilibrium phase of A + HP clinoenstatite = forsterite + water was experimentally investigated at aH2O = 1 in situ. In cold subducting slabs, it is of relevance to transport water to large depths, initiating the formation of dense hydrous magnesium silicate (DHMS). At normal gradients, the huge water amount from this reaction induces important processes within the overlying mantle wedge. We additionally discuss the relevance of this reaction for intermediate-depth earthquake formation.
Read more