Articles | Volume 10, issue 5
https://doi.org/10.5194/se-10-1733-2019
https://doi.org/10.5194/se-10-1733-2019
Research article
 | 
23 Oct 2019
Research article |  | 23 Oct 2019

Deformation mechanisms in mafic amphibolites and granulites: record from the Semail metamorphic sole during subduction infancy

Mathieu Soret, Philippe Agard, Benoît Ildefonse, Benoît Dubacq, Cécile Prigent, and Claudio Rosenberg

Viewed

Total article views: 3,339 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,944 1,259 136 3,339 328 92 122
  • HTML: 1,944
  • PDF: 1,259
  • XML: 136
  • Total: 3,339
  • Supplement: 328
  • BibTeX: 92
  • EndNote: 122
Views and downloads (calculated since 14 Feb 2019)
Cumulative views and downloads (calculated since 14 Feb 2019)

Viewed (geographical distribution)

Total article views: 3,339 (including HTML, PDF, and XML) Thereof 2,734 with geography defined and 605 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (preprint)

Latest update: 01 Nov 2024
Download
Short summary
This study sheds light on the mineral-scale mechanisms controlling the progressive deformation of sheared amphibolites from the Oman metamorphic sole during subduction initiation and unravels how strain is localized and accommodated in hydrated mafic rocks at high temperature conditions. Our results indicate how metamorphic reactions and pore-fluid pressures driven by changes in pressure–temperature conditions and/or water activity control the rheology of mafic rocks.