OJG  Vol.5 No.9 , September 2015
Structural Style in the Khalfani Anticline, Coastal Fars, Zagros Fold-Thrust Belt
The Khalfani anticline is located in the Coastal Fars (Zagros, adjacent Persian Gulf). This anticline with Northwest-Southeast trend is a fault bend fold. In the study area, the Khalfani anticline has increased elevation from West to East with three distinct humps. The major faults in the study area are the Hendurabi and the Razak sinistral strike slip faults. Because analysis of fold and their folding s in different parts system is important, the analysis of folding elements is necessary for structural studies. The main aim of this research is structural analysis based on fold elements in the Khalfani anticline. This analysis is important for progress in hydrocarbons exploration in the Coastal Fars area. In this research, we used Tectonics FP and Global Mapper Software for preparing some data in our study. In addition, we used the common classification of folds for our research. Based on given results, the folding pattern of this anticline has indicated that the fold is same in different parts of the Khalfani anticline. In the study area, based on classifications of fold in different methods, fold is same together. Fold, with close sideways requires special attention as structural view; then the Khalfani Anticline with close in all parts has special deformation and folding . It seems that in the study area, folding and variation of structural have been created by effect of the Razak and the Hendurabi sinistral strike slip fault. Because these faults are basement or deep-seated faults, special folding and special deformation can be formed in the study area. In addition, the Khalfani anticline in the study area has restricted within the Razak and the Hendurabi sinistral strike slip faults.

Cite this paper
Baghbanan, A. , Maleki, Z. and Pourkemani, M. (2015) Structural Style in the Khalfani Anticline, Coastal Fars, Zagros Fold-Thrust Belt. Open Journal of Geology, 5, 655-665. doi: 10.4236/ojg.2015.59058.
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