تحلیل ساختارهای شکننده ارتفاعات شمال خاور رفسنجان

The heights in the east northern part of Rafsanjan- with a north west to southeast trend are mainly made up of folded and broken sedimentary rocks wich were formed from precomberian to Neogen the most important structure of this area is Davaran right-turned strkie slip fault with according to its geometrical position and mechanism, seems to be the main factor of deformation in this area field observations and Digital Process on the data satellite prove the conformity between the faults in this region and the .Y breakages in a shearzone also the trend and mechanism of these faults as compared with the trend of the major zon of the deformation comfirm the mechanism of convergent strike slip fault in this area

کلید واژه ها: کرمان