Map was generated usingto evaluate groundwater possible is illustrated in Fighole information. The methodology employed overlay analysis and additional validated with borehole information.two. ure The methodology used to evaluate groundwater prospective is illustrated in Figure two.Figure two. Flowchart from the groundwater prospective assessment methodology. Figure two. Flowchart of your groundwater prospective assessment methodology.two.1. Study Location The study area is positioned in central Mianyang City, Sichuan Province, China (Figure 1). Its longitude range is from 104 11 E to 104 38 E, and the latitude range is from 31 34 N2.1 Study Location The study area is located in central Mianyang City, Sichuan Province, China (Figure 1). Its longitude variety is from Gamma-glutamylcysteine Technical Information 1041’E to 1048’E , and the latitude range is from 314’N to 32 . The elevation ranges from a high of 2345 m in the northwest to a low of four of 19 501 m within the southeast. The area is dominated by the northeast-oriented Longmenshan Fault, using the Songpan-Ganzi Fold Program inside the west along with the Sichuan Basin inside the east. Complicated tectonic deformation has weakened the tectonic pressure field in the region [47]. According elevation ranges from a higher of 2345 in the Geological Environment m in to 32 N. Theto the hydrogeological map obtained m in the northwest to a low of 501 Monitoring Institute of China Geological by the northeast-oriented Longmenshan water is disthe southeast. The region is dominated Survey, a large carbonate karst fissure of Fault, with tributed within the central portion, and bedrock fissure water is primarily distributed inside the norththe Songpan-Ganzi Fold Technique in the west as well as the Sichuan Basin within the east. Complicated west of your fracture zone; unconsolidated strata pore water and clastic fracture water are tectonic deformation has weakened the tectonic strain field within the area [47]. According to mainly distributed map obtained from south (Figure three) [48]. the hydrogeological inside the northeast andthe Geological Environment Monitoring Institute The area experiences a large carbonate karst fissure of water with a mean annual of China Geological Survey,a humid, subtropical climatic condition is distributed in the temperature of bedrock fissure water is mostly distributed in the northwest on the fracture central aspect, and 16 and annual rainfall of more than 1100 mm. Three Fujiang River tributaries flow via the area, namely, the and clastic fracture Subao River, and the Tongkou zone; unconsolidated strata pore waterAnchang River, the water are mainly distributed in River. the northeast and south (Figure three) [48].Remote Sens. 2021, 13,Figure Groundwater sorts within the study area. Figure 3.three. Groundwater types in the study region.two.2. The region experiences a humid, subtropical climatic condition using a mean annual Evaluation System temperature of 16 Methodannual rainfall of more than 1100 mm. Three Fujiang River tributaries two.2.1. Weighting C and and Overlay Analysis flow through the region, namely, the Anchang River, the Subao River, and the Tongkou River. AHP, a helpful multicriteria Naftopidil Technical Information decision-making technique, was utilised to assign weights to every established issue 2.two. Evaluation Strategy for affordable assessment [39]. We applied previous information to categorize the System and Overlay Evaluation two.2.1. Weightingoccurrence and movement of groundwater hierarchically and examine it through the AHP approach [49]. The following measures had been adapted to assign weights of AHP, a beneficial multicriteria decision-making process, was used to assign weights for the aspects.