The kinematics of the Dasht-e Bayaz earthquake fault during Pliocene-Quaternary: Implications for the tectonics of eastern Central Iran

Author:

Baniadam Fariborz,Shabanian EsmaeilORCID,Bellier Olivier

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference108 articles.

1. Evolution of the stress field in the Tehran region during the Quaternary;Abbassi,1999

2. Faulting and folding in quaternary deposits of Tehran’s piedmont (Iran);Abbassi;J. Asian Earth Sci.,2009

3. Quaternary state of stress in the Mahneshan-Mianeh sedimentary basin, NW Iran;Aflaki;Sci. Q. Geosci.,2017

4. Signatures of deformation related to the Plio-Quaternary state of stress in the Mahneshan-Mianeh Basin (NW Iran);Aflaki;Iran. J. Seismol. Earthquake Eng.,2018

5. Seismotectonic characteristics of the 2017 Sefid Sang (Mw 6) earthquake;Aflaki;The 18th Iranian Geophysical Conference,2018

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