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Information Journal Paper

Title

SEISMOTECTONIC CHARACTERISTICS OF THE ZARAND REGION WITH SPECIAL REFERENCE TO THE 22 FEB. DAHUIEH (ZARAND) EARTHQUAKE

Pages

  1-8

Abstract

 The Mw 6.4 (Ms 6.5) Dahuiyeh (Zarand) earthquake occurred on February 22, 2005 in KERMAN PROVINCE in south Iran. The earthquake ruptured an INTRA-MOUNTAIN REVERSE FAULT, striking E-W and dipping north at about 60 degree to a depth of about 10 km. It produced a series of coseismic scarps with up to 1m vertical displacement over a total distance of about 13 km, continuous for a 7 km. The line of the coseimic ruptures followed a known geological fault of unknown, but probably pre-late cenozoic age and involved bedding-plane slip where scarp were continuous at the surface. Faults of this type represent serious seismic hazard in Iran and are difficult to assess, because their geomorphologic expression is much less clear than the range-bounding reverse faults, which are common and have been better studied. The intense shaking in ZARAND CITY and neighbouring villages, killing about 612 people of inhabitants of the earthquake area.

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    APA: Copy

    AFSARI FARD, SAEED, & GHORASHI, MANOCHEHR. (2007). SEISMOTECTONIC CHARACTERISTICS OF THE ZARAND REGION WITH SPECIAL REFERENCE TO THE 22 FEB. DAHUIEH (ZARAND) EARTHQUAKE. JOURNAL OF THE EARTH, 2(2), 1-8. SID. https://sid.ir/paper/193024/en

    Vancouver: Copy

    AFSARI FARD SAEED, GHORASHI MANOCHEHR. SEISMOTECTONIC CHARACTERISTICS OF THE ZARAND REGION WITH SPECIAL REFERENCE TO THE 22 FEB. DAHUIEH (ZARAND) EARTHQUAKE. JOURNAL OF THE EARTH[Internet]. 2007;2(2):1-8. Available from: https://sid.ir/paper/193024/en

    IEEE: Copy

    SAEED AFSARI FARD, and MANOCHEHR GHORASHI, “SEISMOTECTONIC CHARACTERISTICS OF THE ZARAND REGION WITH SPECIAL REFERENCE TO THE 22 FEB. DAHUIEH (ZARAND) EARTHQUAKE,” JOURNAL OF THE EARTH, vol. 2, no. 2, pp. 1–8, 2007, [Online]. Available: https://sid.ir/paper/193024/en

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