RECONSTRUCTION OF KUHBANAN FAULT SYSTEM SINCE LATE PLIOCENE, WEST OF BAHABAD, CENTRAL IRAN

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SHAFIEI BAFTI A.; SHAH PASANDZADEH M.; POURKERMANI M.

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Journal: JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY) Year:2007 | Volume:17 | Issue:65 (GEOLOGY ISSUE) Page(s): 111-126

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Title

RECONSTRUCTION OF KUHBANAN FAULT SYSTEM SINCE LATE PLIOCENE, WEST OF BAHABAD, CENTRAL IRAN

Author(s)

SHAFIEI BAFTI A. | SHAH PASANDZADEH M. | POURKERMANI M. | Issue Writer Certificate

Keywords

ACTIVE TECTONICSQ3

GEOMORPHIC INDICESQ3

DRAINAGE RECONSTRUCTIONQ3

CUMULATIVE DISPLACEMENTQ3

SLIP RATEQ3

STRIKE-SLIP FAULTQ3

KUHBANAN FAULT SYSTEMQ3

Abstract

Kuhbanan fault system, as one of the intercontinental faults of central Iran, is recognized by considerable seismogenic activities and modem morphotectonics evidences with a strike-slip (reverse component) motion. According to the geometric and kinematics data, Kuhbanan fault has been divided into 5 segments (S26, S27, S28, S29, S30) in Bahabad region. Measured GEOMORPHIC INDICES of ratio of valley-floor width to valley height (Vf) and morphology of the valley (V) manifest the maximum denudation rate for the S28segment. The mean calculated values of mountain-front sinuosity (Smf) and %facet parameters for different segments of the fault are 1.1 and 83.16, consequently. Regarding to these GEOMORPHIC INDICES, a denudation rate of about 2-4 mmyr-1 is suggested for this region.According to reconstruction of Kuhbanan fault since 360 ka, minimum horizontal CUMULATIVE DISPLACEMENT of 750 m and minimum SLIP RATE of about 2-1.4±0.1mmyr-1 is inferred from well preserved geomorphology in the northern segment of the fault. Applying this horizontal CUMULATIVE DISPLACEMENT causes reconstruction of geomorphic markers such as drainages and shuttered ridges.

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APA: Copy

SHAFIEI BAFTI, A., SHAH PASANDZADEH, M., POURKERMANI, M.,. (2007). RECONSTRUCTION OF KUHBANAN FAULT SYSTEM SINCE LATE PLIOCENE, WEST OF BAHABAD, CENTRAL IRAN. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), 17(65 (GEOLOGY ISSUE)), 111-126. SID. https://sid.ir/paper/70499/en

Vancouver: Copy

SHAFIEI BAFTI A., SHAH PASANDZADEH M., POURKERMANI M.. RECONSTRUCTION OF KUHBANAN FAULT SYSTEM SINCE LATE PLIOCENE, WEST OF BAHABAD, CENTRAL IRAN. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY)[Internet]. 2007;17(65 (GEOLOGY ISSUE)):111-126. Available from: https://sid.ir/paper/70499/en

IEEE: Copy

A. SHAFIEI BAFTI, M. SHAH PASANDZADEH, M. POURKERMANI, an, “RECONSTRUCTION OF KUHBANAN FAULT SYSTEM SINCE LATE PLIOCENE, WEST OF BAHABAD, CENTRAL IRAN,” JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), vol. 17, no. 65 (GEOLOGY ISSUE), pp. 111–126, 2007, [Online]. Available: https://sid.ir/paper/70499/en

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