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Information Journal Paper

Title

MORPHOTECTONIC INDICES OF LALEZAR FAULT IN SOUTH OF BARDSIR

Pages

  103-110

Abstract

 The study area with 56 20-57 longtitude and 29 20-30 latitude is located in 16 km of southern of BARDSIR city. This region from geological point of view is located in Euromie–Dokhtar magmatism zone. The LALEZAR FAULT is one of effective structure in Euromieh–Dokhtar magmatism zone. In order to Lalehzar fault activity, we studied the MORPHOTECTONIC observation. Lalehzar fault with 84 km length is comperssional fault system with strike slip component.There is a limitation of registered seismic activity along the Lalehzar fault, so in order to know the movements that accour along it, we studied MORPHOTECTONIC evidences such as: waterway deviations form, pressure ridges, shutter ridges, waterway clogging, rivers long straight-line, springs and teravertine bedding, UPLIFT and so on.This study shows that there are some UPLIFT and strike slip movments with left lateral component along the LALEZAR FAULT. These types of activity is more effective in centeral part of the fault.

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    • Cite

    APA: Copy

    KHODAMI, A., BOUZARI, S., & SHAFIEI BAFTI, A.. (2010). MORPHOTECTONIC INDICES OF LALEZAR FAULT IN SOUTH OF BARDSIR. JOURNAL OF THE EARTH, 5(1), 103-110. SID. https://sid.ir/paper/193085/en

    Vancouver: Copy

    KHODAMI A., BOUZARI S., SHAFIEI BAFTI A.. MORPHOTECTONIC INDICES OF LALEZAR FAULT IN SOUTH OF BARDSIR. JOURNAL OF THE EARTH[Internet]. 2010;5(1):103-110. Available from: https://sid.ir/paper/193085/en

    IEEE: Copy

    A. KHODAMI, S. BOUZARI, and A. SHAFIEI BAFTI, “MORPHOTECTONIC INDICES OF LALEZAR FAULT IN SOUTH OF BARDSIR,” JOURNAL OF THE EARTH, vol. 5, no. 1, pp. 103–110, 2010, [Online]. Available: https://sid.ir/paper/193085/en

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