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The study is located in the structural zone of Sanandaj-Sirjan. According to the structure this zone form by the collision of the Arabian and Iranian plates, the study area consist of trust and reveres fault. Shahlora Mountain is one of the tectonic effects of the secondary structures in Sanandaj-sirjan. Based on the morphotectonic studies, structural trend of this mountain is accordant with the fault trend of Zagros and also indicated the relationship of this highland with the fault activity. The activity strike slip fault which is geometrically perpendicular to per-existing trust fault, lead to sinsistral and dextral displacements.The displacement rate of motioned fault is attested by structures which are represented in the text.

کلید واژه ها: چهارمحال