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: 2,131 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,453 612 66 2,131 230 61 49
  • HTML: 1,453
  • PDF: 612
  • XML: 66
  • Total: 2,131
  • Supplement: 230
  • BibTeX: 61
  • EndNote: 49
Views and downloads (calculated since 26 Oct 2020)
Cumulative views and downloads (calculated since 26 Oct 2020)

Viewed (geographical distribution)

Total article views: 2,131 (including HTML, PDF, and XML) Thereof 2,049 with geography defined and 82 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 21 Nov 2024
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.