CSIR – National Geophysical Research Institute, Hyderabad, 500007, India
Viewed
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 3,222 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,545
605
72
3,222
108
88
137
HTML: 2,545
PDF: 605
XML: 72
Total: 3,222
Supplement: 108
BibTeX: 88
EndNote: 137
Views and downloads (calculated since 21 Feb 2023)
Cumulative views and downloads
(calculated since 21 Feb 2023)
Total article views: 2,880 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,203
605
72
2,880
108
83
134
HTML: 2,203
PDF: 605
XML: 72
Total: 2,880
Supplement: 108
BibTeX: 83
EndNote: 134
Views and downloads (calculated since 30 Aug 2023)
Cumulative views and downloads
(calculated since 30 Aug 2023)
Total article views: 342 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
342
0
0
342
5
3
HTML: 342
PDF: 0
XML: 0
Total: 342
BibTeX: 5
EndNote: 3
Views and downloads (calculated since 21 Feb 2023)
Cumulative views and downloads
(calculated since 21 Feb 2023)
Viewed (geographical distribution)
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 3,222 (including HTML, PDF, and XML)
Thereof 3,106 with geography defined
and 116 with unknown origin.
Total article views: 2,880 (including HTML, PDF, and XML)
Thereof 2,773 with geography defined
and 107 with unknown origin.
Total article views: 342 (including HTML, PDF, and XML)
Thereof 333 with geography defined
and 9 with unknown origin.
We use numerical models to study the stresses arising from gravitational potential energy (GPE) variations and shear tractions associated with mantle convection in the Zagros–Iran region. The joint models predicted consistent deviatoric stresses that can explain most of the deformation indicators. Stresses associated with mantle convection are found to be higher than those from GPE, thus indicating the deformation in this region may primarily be caused by the mantle, except in eastern Iran.
We use numerical models to study the stresses arising from gravitational potential energy (GPE)...