...Reza Mansouri; Alessia Maggi; Jean-Paul Montagner Abstract The 20 December 2010 M w 6.3 earthquake near Rigan in southeastern Iran occurred on a previously unknown active fault in the southern Lut block. Its position was inferred by Walker et al. (2013) using Interferometric Synthetic Aperture...

...Mehdi Rezapour; Amir Mohsenpur Abstract The 20 December 2010 M w 6.5 Rigan earthquake that occurred in southeastern Iran was followed by an extensive aftershock sequence. A six‐station portable seismographic network was deployed by the Institute of Geophysics at the University of Tehran around...

...Maryam Safarshahi; Mehdi Rezapour; Hosein Hamzehloo Abstract We studied the 20 December 2010 Rigan earthquake that occurred in southeastern Iran, using the ground‐motion simulation based on the stochastic finite‐fault model. This earthquake was recorded by 23 stations. The method requires region...

..., a moderate earthquake with a magnitude of M w  6.3 occurred in the Rigan area. The causative fault of the 2010 earthquake is not clearly identifiable on the near‐surface geomorphology ( Walker et al. , 2013 ). The epicenter of the event was associated with a hidden part of the Kahurak fault ( Maleki et...

... Lucas P. Moreira, Michael J. Friedel, and George S. França Earthquakes Triggered by Hydraulic Fracturing in South‐Central Oklahoma Austin A. Holland The 2010 M w  6.5 Rigan, Iran, Earthquake Aftershock Sequence Mehdi Rezapour and Amir Mohsenpur A New Zealand‐Specific...

... Stochastic Finite Fault Modeling of Ground Motion for the 2010 Rigan Earthquake, Southeastern Iran Maryam Safarshahi, Mehdi Rezapour, and Hosein Hamzehloo The Analysis of Long‐Term Frequency and Damping Wandering in Buildings Using the Random Decrement Technique Ali Mikael, Philippe Gueguen, Pierre...

... faults. However, several recent earthquakes have ruptured complex fault systems with multiple fault segments occurring in places with poorly mapped faults. Examples include the 2010–2011 moment magnitude M w  6.5–6.2 Rigan, Iran, strike‐slip rupture sequence ( Rezapour and Mohsenpur, 2013...

... , 173 – 192 , doi: 10.1785/0120200172 . Safarshahi M. Rezapour M. , and Hamzehloo H. 2013 . Stochastic finite fault modeling of ground motion for the 2010 Rigan earthquake, southeast Iran , Bull. Seismol. Soc. Am. 103 , 223 – 235 . Wessel P. , and Smith W. H. F...

.... Shomali Z. H. Riahi M.‐A. ( 2013 ). An application of ambient noise and earthquake tomography in the Rigan area, southeast of Iran , Seismol. Res. Lett. 84 , no.  6 , 1014–1020 , doi: 10.1785/0220130044 . Shomali Z. H. Shirzad T. ( 2015 ). Crustal structure of Damavand...

... and surrounding areas ( Zafarani et al. , 2009 ; Nowroozi, 2010 ; Zolfaghari, 2014 ). However, up‐to‐date national and regional hazard assessments are not available, at a time when seismic‐hazard assessments at this level play a major rule for planning global activities aimed at earthquake risk reduction...

... . Shirzad T. Shomali Z. H. Riahi M.‐A. ( 2013 ). An application of ambient noise and earthquake tomography in the Rigan area, southeast of Iran , Seismol. Res. Lett. 84 , no.  6 , 1014 – 1020 , doi: 10.1785/0220130044 . Snieder R. K. ( 2004 ). Extracting the Green’s function...

.... In this article, we revisit earthquake seismic data from a study by Safarshahi et al. (2013) , who considered body S waves in Rigan region of southeastern Iran (Fig.  1 ). The dataset consists of 31 records from the 20 December 2010 and 27 January 2011 Rigan earthquakes with magnitudes M w ≈ 6.5...

...-1986-7 . Najafi M. N. Rahimi‐Majd M. , and Shirzad T. 2020 . Avalanches on the complex network of Rigan earthquake , EPL 130 , 20001 , doi: 10.1209/0295-5075/130/20001 . Nakano N. Osanai Y. Owada M. Nam T. N. Charusiri P. , and Khamphavong K. 2013...

.... A. Elliott J. R. Fielding E. J. Ghods A. R. Ghoraishi M. Jackson J. Nazari H. Nemati M. , and Oveisi B. , et al. 2013 . The 2010‐2011 South Rigan (Baluchestan) earthquake sequence and its implications for distributed deformation and earthquake hazard in southeast Iran...

... from body‐wave modeling ( Nissen et al. , 2010 ), and for the 2006 Fin earthquake sequence, of which the largest event was M w  5.7, the geodetic estimate is 50% higher than the body‐wave estimate ( Roustaei et al. , 2010 ). Lohman and Simons (2005) found geodetic moments up to six times...