A study on thin sections, core, and dynamic reservoir in the considered region indicates that dolomite, as one of the diagenetic processes, plays an important role in determining reservoir characteristic. With regard to the available studies, it is obvious that porosity of Sarvak reservoir varies between 2.5 to 3 percent and its estimated permeability is between 0.01- 10 millidarcy. According to the research, one ramp type carbonate platform has been determined in the studied field of Sarvak formation. The formation carbonate facieses consist of framework grains. The framework grains consist of skeletal fragments such as foraminifers, brachiopods, echinoderms, algal fragments, ploids, and minerals. Moreover, the minerals consist of calcite, dolomite, anhydrate, cloy minerals, components which include organic materials, and finally calcareous matrix which is formed in dolomite samples of very fine anhedral and subhedral dolomite crystals.