The Kushmor (Turshiz) 1903 and Torbut-e Hcidnriyeh (Sollth) 1923 earthquakes in Central Khornssnn (Iran)

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The Salmas (Iran) earthquake of May 6th, 1930

Field investigations and bibliographical research into
 the little-known but important Salmas earthquake in Northwest Azarbaijan
 (Iran) provided the following results. The morning before the earthquake,
 a foreshock (Mb — 5.4) centered, as the main shock, in the Salmas
 Plain, killed about 25 people and incited a great part of the population to
 spend the following night out of doors. The main shock (Mb = 7.3) occurred
 the following night, on 6 May 1930 at 22h34m27s GMT and destroyed about
 60 villages and 40 churches, killing about 2514 people, both in the Salmas
 Plain and in the surrounding mountains. Its macroseismic epicentre was
 at approximately 3S.15N 44.70E. The main shock was associated with 2
 surface faults, with a maximum horizontal displacement of 4 m and vertical
 displacement of over 5 m; the combined action of these faults was a
 relative lowering, and a displacement to the east, of the Salmas Plain. Two
 days later, the strongest aftershock destroyed one village at the northern
 edge of the Salmas Plain

The Babol-Kenar (1971) earthquake and the seismotectonics of the Central Alborz (Iran)

The Babol-Kenar earthquake (9tli August, 1971) was arelatively minor event compared to previous catastrophic earthquakes inthe Central Alborz mountains of northern Iran. It's study however, isimportant for the understanding of the seismicity of a region which hasalready experienced two large earthquakes during this century and whichcould be entering a phase of renewed seismic activity. The p a t t e r n deducedfrom the sequence of all recorded earthquakes in the region outlines thestructural units of the Central Alborz and suggests the existence of seismotectonicprovinces which are alternatively active and quiescent