Geophysical Journal International Geophys. J. Int. (2010) 182, 1577–1602 doi: 10.1111/j.1365-246X.2010.04705.x The Rudbar¯ Mw 7.3 earthquake of 1990 June 20; seismotectonics, coseismic and geomorphic displacements, and historic earthquakes of the western ‘High-Alborz’, Iran Manuel Berberian1 and Richard Walker2 11224 Fox Hollow Drive, Toms River, NJ 08755-2179, USA. E-mail:
[email protected] 2Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK. E-mail:
[email protected] Accepted 2010 June 17. Received 2010 June 17; in original form 2008 December 21 Downloaded from https://academic.oup.com/gji/article/182/3/1577/600044 by guest on 01 October 2021 SUMMARY The Rudbar¯ earthquake of 1990 June 20, the first large-magnitude earthquake with 80 km left-lateral strike-slip motion in the western ‘High-Alborz’ fold-thrust mountain belt, was one of the largest, and most destructive, earthquakes to have occurred in Iran during the instrumental period. We bring together new and existing data on macroseismic effects, the rupture characteristics of the mainshock, field data, and the distribution of aftershocks, to provide a better description of the earthquake source, its surface ruptures, and active tectonic characteristics of the western ‘High-Alborz’. The Rudbar¯ earthquake is one of three large magnitude events to have occurred in this part of the Alborz during recorded history. The damage distribution of the 1485 August 15 Upper Polrud earthquake suggests the east–west Kelishom left-lateral fault, which is situated east of the Rudbar¯ earthquake fault, as a possible source.