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Information Journal Paper

Title

FRACTURES ANALYSIS IN LALI ANTICLINE, SW IRAN

Pages

  19-35

Abstract

 The LALI ANTICLINE is located about 60-Km northeast of Shushtar in SW Iran and in the Dezful embayment zone. In this research, subsurface data have been used for analysis of folding and fracturing mechanisms in the studied area. Due to presence of a THRUST FAULT in the southern limb (forelimb) of LALI ANTICLINE, it is suggested that this anticline is a fault propagation fold. Geometrical analysis methods, including inscribed circles analysis, derivative from subsurface structural maps, calculation axial curvature amount of reservoir structure and relative frequency of FRACTUREs method (RFF), are shown that the SW limb (forelimb) of the anticline has higher potential FRACTURE density.

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    Cite

    APA: Copy

    RAMEZANI, A., ALAVI, S.A., & HAJIALIBEIGI, H.. (2012). FRACTURES ANALYSIS IN LALI ANTICLINE, SW IRAN. IRANIAN JOURNAL OF GEOLOGY, 6(23), 19-35. SID. https://sid.ir/paper/129500/en

    Vancouver: Copy

    RAMEZANI A., ALAVI S.A., HAJIALIBEIGI H.. FRACTURES ANALYSIS IN LALI ANTICLINE, SW IRAN. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2012;6(23):19-35. Available from: https://sid.ir/paper/129500/en

    IEEE: Copy

    A. RAMEZANI, S.A. ALAVI, and H. HAJIALIBEIGI, “FRACTURES ANALYSIS IN LALI ANTICLINE, SW IRAN,” IRANIAN JOURNAL OF GEOLOGY, vol. 6, no. 23, pp. 19–35, 2012, [Online]. Available: https://sid.ir/paper/129500/en

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