Active deformation and seismicity of Dorouneh Fault System in north of Central Iran microplate emphasizing on 1903 Torshiz and 1923 Kaj-Derakht earthquakes

رخساره‌های رسوبی

Article 2, Volume 1, Issue 1, February 2009, Pages 1-18   

Document Type: مقالات پژوهشی

DOI: 10.22067/sed.facies.v1i1.728

Authors

Hamid Reza Javadi^{* 1}; Majid Shahpasandzadeh²; Mohammad Rza Ghassemi¹; Marzieh Estrabi Ashtiani¹

¹Geological Survey of Iran

²International Center for Science and High Technology, Kerman

Abstract

Dorouneh Fault System, as an active fault in Iranian Plateau, plays an important role in deformation and geomorphology of the region. This fault has caused some earthquakes in the 20th century. Detail study of Dourouneh fault's seismic characteristics indicates that in spite of Dorouneh Fault's high movement in Recent time, number of earthquakes and their magnitude is low that may be resultant of low slip rate, long recurrence interval and occurrence of creep on the fault. On the other hand, there are some witnesses that are indication of earthquake occurrence along Dourouneh fault which are accompanied with surface rupture.

Keywords

Dorouneh Fault System; Seismicity; Morphotectonics

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