摘要：The study area is located in the Dezful Embayment division structure is known. In this chapter, first, in order to analyze the structure of anticlinal folds, the characteristics of anticlinal belts in mountainous belts and the general features of anticlines of Zagros , its anticlinal belts and the synclines or curves of Dezfol have been described.It was determined the geometry of the Zagros deformation front and front of the basin is controlled by minimum two different structural parameters(1) Mechanical nature of the separation rule shortening ZFTB and(2) Reactivation of basement faults effective in the tectonic model of crustal thickness. Structural style of the Dezful Embayment associated is with faulting and folding sliding surface. In the area of the sliding surface to evaporate a Gachsaran formation has created. It seems that the main reason for folding uncooperative is sliding between Gachsaran and Asmari the by the difference in level viscosity
