In this study, the Makran zone in southern Iran and Pakistan has been evaluated by considering the seismicity concepts of the Gutenberg-Richter relationship. The statistical properties of earthquakes (epicenter distribution and magnitude of earthquakes and faults) have been studied in accordance with the power law of the characteristic space-time distribution (density of time and space distribution). The basis of calculation is the seismic dimension parameters (b-value), which is calculated based on the maximum probability. Unlike other methods, in this method, the temporal and spatial distribution of parameters, the cumulative properties of the data (inherent dimension) and the level of tectonic stress in the area related to different tectonic seismic processes are considered. In order to calculate these parameters, seismic data from different databases (internal and external) have been used. The correlation dimension b (0.8<b<1.6) value, computed from the earthquake epicenter and magnitude distributations show significant temporal and spatial variation related with seismo tectonic feature of fault zones.