A Reconnaissance Report on two Iran, Makran Earthquakes Iran, Makran Earthquakes ; 16 April 2013, Mw7.8, Gosht (Saravan) and 11 May 2013 Irar (Goharan), Bashagard, SE of Iran Authors and Affiliations Mehdi ZARE1, Anooshiravan Ansari2, Heydar Heydari3, Mo- hammad P.M. Shahvar4, Mehdi Daneshdust5, Majid Mahdi- an6, Fereidoun Sinaiean7, Esmail Farzanegan8 and Hossein Mirzaei-Alavijeh9 1International Institute of Earthquake Engineering and Seis- mology (IIEES), Tehran, Iran,
[email protected], (Member EERI) 2IIEES,
[email protected] 3Relief & Rescue Organization, Iranian Red Crescent Socie- ty, Tehran, Iran 4IIEES,
[email protected] 5Islamic Azad University, Science and Research Branch, Tehran, Iran (
[email protected]) 6Institute of Geophysics, University of Tehran (
[email protected]) 8,9Building and Housing Research Center, Tehran, Iran, (7:
[email protected]), (8:
[email protected]) and (9:
[email protected]). report design by Brijhette Farmer, EERI Introduction Iran has experienced two strong earthquakes, in April and May 2013, in the Makran ranges within 25 days. The first earthquake occurred on 16 April 201s3, with Mw7.8 the Sa- ravan region in the eastern end of Iranian Makran. The se- cond one happened in western Makran, on 11 May 2013, with Mw6.2, in Irar, Bashagard region, close to the Minab-Zendan Fault zone. This report tries to summarize the reconnaissance reports and early seismological and earthquake engineering evaluations on these two strong earthquakes. Figure-1: The epicenter of the Gosht (Savaran), 1. Seismicity of the Makran belt. SE Iran, western Pakistan, by Norwegian Refu- gee Council (from https://www.relief-web.int).