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Information Journal Paper

Title

GEOMETRIC ANALYSIS OF A FAULT-RELATED FOLDING TO AN ACTIVE BLIND FAULT, ANARAN ANTICLINE, SW IRAN

Pages

  71-83

Abstract

 The ANARAN anticline is located between Lurestan (in the north) and Dezful Embayment (in the south) zones in the ZAGROS fold-thrust belt. This anticline and adjacent anticlines are affected by the BALARUD BLIND THRUST fault zone, which is a part of Mountain Front Fault. The Mountain Front Fault is a major topographic front that can be traced along the ZAGROS folded-thrust belt in the Izeh, Fars, Lurestan and Dezful Embayment. The field observations, analyses of the geometric parameters and comparison of the anticline with the theoretical fault-related folding models suggest that the ANARAN anticline is a fault-bend fold mode Õ that is sheared by BALARUD BLIND THRUST fault zone.

Cites

References

Cite

APA: Copy

HAJI ALI BEYGI, H., ALAVI, SEYED AHMAD, EFTEKHARNEZHAD, J., & MOKHTARI, MOHAMMAD. (2009). GEOMETRIC ANALYSIS OF A FAULT-RELATED FOLDING TO AN ACTIVE BLIND FAULT, ANARAN ANTICLINE, SW IRAN. IRANIAN JOURNAL OF GEOLOGY, 2(8), 71-83. SID. https://sid.ir/paper/129342/en

Vancouver: Copy

HAJI ALI BEYGI H., ALAVI SEYED AHMAD, EFTEKHARNEZHAD J., MOKHTARI MOHAMMAD. GEOMETRIC ANALYSIS OF A FAULT-RELATED FOLDING TO AN ACTIVE BLIND FAULT, ANARAN ANTICLINE, SW IRAN. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2009;2(8):71-83. Available from: https://sid.ir/paper/129342/en

IEEE: Copy

H. HAJI ALI BEYGI, SEYED AHMAD ALAVI, J. EFTEKHARNEZHAD, and MOHAMMAD MOKHTARI, “GEOMETRIC ANALYSIS OF A FAULT-RELATED FOLDING TO AN ACTIVE BLIND FAULT, ANARAN ANTICLINE, SW IRAN,” IRANIAN JOURNAL OF GEOLOGY, vol. 2, no. 8, pp. 71–83, 2009, [Online]. Available: https://sid.ir/paper/129342/en

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