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: 4,628 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
3,483
1,006
139
4,628
158
191
227
HTML: 3,483
PDF: 1,006
XML: 139
Total: 4,628
Supplement: 158
BibTeX: 191
EndNote: 227
Views and downloads (calculated since 21 Feb 2023)
Cumulative views and downloads
(calculated since 21 Feb 2023)
Total article views: 3,703 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,571
994
138
3,703
154
155
205
HTML: 2,571
PDF: 994
XML: 138
Total: 3,703
Supplement: 154
BibTeX: 155
EndNote: 205
Views and downloads (calculated since 30 Aug 2023)
Cumulative views and downloads
(calculated since 30 Aug 2023)
Total article views: 925 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
912
12
1
925
36
22
HTML: 912
PDF: 12
XML: 1
Total: 925
BibTeX: 36
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: 4,628 (including HTML, PDF, and XML)
Thereof 4,443 with geography defined
and 185 with unknown origin.
Total article views: 3,703 (including HTML, PDF, and XML)
Thereof 3,529 with geography defined
and 174 with unknown origin.
Total article views: 925 (including HTML, PDF, and XML)
Thereof 914 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)...
