Articles | Volume 12, issue 4
https://doi.org/10.5194/se-12-817-2021
https://doi.org/10.5194/se-12-817-2021
Research article
 | 
15 Apr 2021
Research article |  | 15 Apr 2021

Analytical solution for residual stress and strain preserved in anisotropic inclusion entrapped in an isotropic host

Xin Zhong, Marcin Dabrowski, and Bjørn Jamtveit

Viewed

Total article views: 3,345 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,331 902 112 3,345 308 127 161
  • HTML: 2,331
  • PDF: 902
  • XML: 112
  • Total: 3,345
  • Supplement: 308
  • BibTeX: 127
  • EndNote: 161
Views and downloads (calculated since 26 Oct 2020)
Cumulative views and downloads (calculated since 26 Oct 2020)

Viewed (geographical distribution)

Total article views: 3,345 (including HTML, PDF, and XML) Thereof 3,193 with geography defined and 152 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 24 Aug 2026
Download
Short summary
Elastic thermobarometry is an useful tool to recover paleo-pressure and temperature. Here, we provide an analytical model based on the Eshelby solution to calculate the residual stress and strain preserved in a mineral inclusion exhumed from depth. The method applies to ellipsoidal, anisotropic inclusions in infinite isotropic hosts. A finite-element method is also used for a facet effect. Volumetrically averaged stress is shown to be a good proxy for the overall heterogeneous stress stage.
Share