Journal cover Journal topic
Solid Earth An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 2.380 IF 2.380
  • IF 5-year value: 3.147 IF 5-year
    3.147
  • CiteScore value: 3.06 CiteScore
    3.06
  • SNIP value: 1.335 SNIP 1.335
  • IPP value: 2.81 IPP 2.81
  • SJR value: 0.779 SJR 0.779
  • Scimago H <br class='hide-on-tablet hide-on-mobile'>index value: 32 Scimago H
    index 32
  • h5-index value: 31 h5-index 31
Volume 9, issue 3
Solid Earth, 9, 821–831, 2018
https://doi.org/10.5194/se-9-821-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Solid Earth, 9, 821–831, 2018
https://doi.org/10.5194/se-9-821-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 20 Jun 2018

Research article | 20 Jun 2018

The seismogenic fault system of the 2017 Mw 7.3 Iran–Iraq earthquake: constraints from surface and subsurface data, cross-section balancing, and restoration

Stefano Tavani et al.
Viewed  
Total article views: 2,586 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,996 550 40 2,586 44 39
  • HTML: 1,996
  • PDF: 550
  • XML: 40
  • Total: 2,586
  • BibTeX: 44
  • EndNote: 39
Views and downloads (calculated since 19 Mar 2018)
Cumulative views and downloads (calculated since 19 Mar 2018)
Viewed (geographical distribution)  
Total article views: 2,370 (including HTML, PDF, and XML) Thereof 2,334 with geography defined and 36 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Cited  
Saved (final revised paper)  
No saved metrics found.
Saved (discussion paper)  
No saved metrics found.
Discussed (final revised paper)  
Discussed (discussion paper)  
No discussed metrics found.
Latest update: 22 Aug 2019
Publications Copernicus
Download
Short summary
A balanced cross section across the hypocentre of the 2017 Iran–Iraq Mw 7.3 earthquake is presented. The structural style of the area is characterised by inversion tectonics with partial decoupling between the basement and the 10 km thick sedimentary cover. The main shock is located along a low-dipping lateral ramp of the Mountain Front Fault. The balanced cross section indicates that the Mountain Front Fault is the only fault where an Mw 7.3 earthquake may occur.
A balanced cross section across the hypocentre of the 2017 Iran–Iraq Mw 7.3 earthquake is...
Citation