Letouzey, J. and Sherkati, S. (2004) Salt Movement, Tectonic Events, and Structural Style in the Central Zagros Fold and Thrust Belt (Iran). Proceedings of the 24th Annual Gulf Coast Section SEPM Foundation, Interactions and Bob F. Perkins Research Conference on Salt Sediments Hydrocarbon Prospectivity, Houston, 5-8 December 2004, 535-554.

has been cited by the following article:

• TITLE: Structural Style in the Khalfani Anticline, Coastal Fars, Zagros Fold-Thrust Belt

  AUTHORS: Arezo Baghbanan, Zahra Maleki, Mohsen Pourkemani

  KEYWORDS: Khalfani Anticline, Structural Style, Hendurabi and Razak Faults

  JOURNAL NAME: Open Journal of Geology, Vol.5 No.9, September 29, 2015

  ABSTRACT: 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 styles in different parts system is important, the analysis of folding style elements is necessary for structural studies. The main aim of this research is structural style analysis based on fold style 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 style is same in different parts of the Khalfani anticline. In the study area, based on classifications of fold in different methods, fold style is same together. Fold, with close sideways requires special attention as structural view; then the Khalfani Anticline with close style in all parts has special deformation and folding style. It seems that in the study area, folding style and variation of structural style 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 style 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.