As the second supplier of world's copper source, Sedimentary-Rock Hosted Copper (SHC) deposits are formed in hydrologically closed basins. In Central Iran, Red-bed type SHCs are concentrated in the contact of red and gray Garadu Formation sandstone. Many SHC deposit and mineral outcrops have been reported in the western and northern Lut block, central Iran. The mentioned area (Kashmar-Kerman and Tabas block) with a north-south trend, is known as Ravar-Tabas SHC Belt, but its exact location, width and border have not been determined yet. In this study, SHC's genesis and tectonic setting is explained and then the tectonic setting and geology of the Central Iran block are evaluated. An area of some 161,000 square km has been chosen (i.e., Kashmar-Kerman Zone and Lut block), as well as another 100quare km surrounding the Ravar and Tabas towns. Geological data (geologic maps and stratigraphic columns) were assembled and prepared for mapping potential sediment formations, and estimation its extended under the ground. All Garadu sandstone and its equivalents, were selected on the maps, then using stratigraphic columns the spread of these bedded layers was extrapolated, in this way a map of geologically (surface and burial) promising area was derived. In addition, the catchment areas were determined by topographic data. Then the total thickness of the Cretaceous to Quaternary sedimentary rocks (measured by geologic sections in some points) were extracted from the original digital elevation model (DEM) and the DEM of Jurassic surface was estimated Then, the Jurassic catchment was modeled using this DEM. In the next step, time-reversed tectonic data (major faults information) was applied over the Jurassic catchment border (by observational logic and Move software), the result was a reshaped catchment border. Then, the applied tectonic Jurassic basin and achieved geologic map were fitted together and compared with each other, so the promising geological map was verified and corrected at 3 points Finally, 23 field-checked deposit coordinates were located on the corrected and final map for validation checking, 18 points were settled inside the border and the rest were located outside the border (because these 5 targets belong to another zone or unknown tectonic events). The final concluded border map is presented at the end, and complementary studies (Remote sensing, geochemistry, sulfide supplier amounts such as organic materials, new first place proposal area, tectonic controllers, detailed geology and stratigraphy) have been suggested for improving this study in future