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: 4,331 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
3,272
965
94
4,331
140
143
185
HTML: 3,272
PDF: 965
XML: 94
Total: 4,331
Supplement: 140
BibTeX: 143
EndNote: 185
Views and downloads (calculated since 21 Feb 2023)
Cumulative views and downloads
(calculated since 21 Feb 2023)
Total article views: 3,432 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,386
953
93
3,432
136
108
163
HTML: 2,386
PDF: 953
XML: 93
Total: 3,432
Supplement: 136
BibTeX: 108
EndNote: 163
Views and downloads (calculated since 30 Aug 2023)
Cumulative views and downloads
(calculated since 30 Aug 2023)
Total article views: 899 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
886
12
1
899
35
22
HTML: 886
PDF: 12
XML: 1
Total: 899
BibTeX: 35
EndNote: 22
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: 4,331 (including HTML, PDF, and XML)
Thereof 4,146 with geography defined
and 185 with unknown origin.
Total article views: 3,432 (including HTML, PDF, and XML)
Thereof 3,258 with geography defined
and 174 with unknown origin.
Total article views: 899 (including HTML, PDF, and XML)
Thereof 888 with geography defined
and 11 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)...
