Iranian earthquakes, a uniform catalog with moment magnitudes

• Published in: Journal of seismology 2013-07, Vol.17 (3), p.897-911
• Main Authors: Karimiparidari, Sepideh, Zaré, Mehdi, Memarian, Hossein, Kijko, Andrzej
• Format: Article
• Language: English
• Subjects: Boundaries; Earth and Environmental Science; Earth Sciences; Earth, ocean, space; Earthquakes; Earthquakes, seismology; Engineering and environment geology. Geothermics; Exact sciences and technology; Geophysics/Geodesy; Geotechnical Engineering & Applied Earth Sciences; Hydrogeology; Internal geophysics; Mountains; Natural hazards: prediction, damages, etc; Original Article; Position (location); Priorities; Seismic activity; Seismic hazard; Seismic phenomena; Seismic zones; Seismology; Structural Geology
• ISSN: 1383-4649; 1573-157X
• DOI: 10.1007/s10950-013-9360-9

A uniform earthquake catalog is an essential tool in any seismic hazard analysis. In this study, an earthquake catalog of Iran and adjacent areas was compiled, using international and national databanks. The following priorities were applied in selecting magnitude and earthquake location: (a) local catalogs were given higher priority for establishing the location of an earthquake and (b) global catalogs were preferred for determining earthquake magnitudes . Earthquakes that have occurred within the bounds between 23–42° N and 42–65° E, with a magnitude range of M W 3.5–7.9, from the third millennium BC until April 2010 were included. In an effort to avoid the “boundary effect,” since the newly compiled catalog will be mainly used for seismic hazard assessment, the study area includes the areas adjacent to Iran. The standardization of the catalog in terms of magnitude was achieved by the conversion of all types of magnitude into moment magnitude, M W , by using the orthogonal regression technique. In the newly compiled catalog, all aftershocks were detected, based on the procedure described by Gardner and Knopoff (Bull Seismol Soc Am 64:1363–1367, 1974 ). The seismicity parameters were calculated for the six main tectonic seismic zones of Iran, i.e., the Zagros Mountain Range, the Alborz Mountain Range, Central Iran, Kope Dagh, Azerbaijan, and Makran.