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: 3,944 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
3,114
752
78
3,944
127
123
163
HTML: 3,114
PDF: 752
XML: 78
Total: 3,944
Supplement: 127
BibTeX: 123
EndNote: 163
Views and downloads (calculated since 21 Feb 2023)
Cumulative views and downloads
(calculated since 21 Feb 2023)
Total article views: 3,086 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,268
740
78
3,086
123
90
143
HTML: 2,268
PDF: 740
XML: 78
Total: 3,086
Supplement: 123
BibTeX: 90
EndNote: 143
Views and downloads (calculated since 30 Aug 2023)
Cumulative views and downloads
(calculated since 30 Aug 2023)
Total article views: 858 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
846
12
0
858
33
20
HTML: 846
PDF: 12
XML: 0
Total: 858
BibTeX: 33
EndNote: 20
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: 3,944 (including HTML, PDF, and XML)
Thereof 3,828 with geography defined
and 116 with unknown origin.
Total article views: 3,086 (including HTML, PDF, and XML)
Thereof 2,979 with geography defined
and 107 with unknown origin.
Total article views: 858 (including HTML, PDF, and XML)
Thereof 849 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)...