Recognition of Source areas of sand dunes is very important in wind erosion control projects. Due to the difficultes in application of traditional methods in recognition and determination of the share of sediment Sources in sediment production, fingerprinting methods, sediment tracery or in other wards, Source identification are alternative and suitable methods which are considered by different researches. In this method, by investigation of physical and chemical characteristics of sediments, rocks and soils of different Sources, the Source areas of sediment are determined.In this research, sediment tracery by geochemical elements, Source areas and the shares of these Sources in eolian sediment production in one of the most important eolian critical centers of sistan plain were identified. First, granolumetric and mineralogical studies were performed on eolian sediments of sistan province. then, step-wise Source identification method was performed on Niatak eolian sediments. Then. by using determination analysis method and suitable composition of geochemical elements, Organic carbon, Phosphorous and Nitrogen which can differentiate lithological, land use and geomorphological units in Niatak critical center and by using composite multivariate methods, the importantance and share of sediment Sources were determined. The results indicated that transport distances have been between 20-50 kilometers and the most important Sources were sediments of Hamon lake and then barren lands that 92% of particles have originate from Hamon lake and River bed and 69% of particles from barren lands.87% of particles have originate from NQts unit (upper Miocene– Pliocene fine – grained alluvial sediments of Hamon lake), having the highest share and QK unit (the youngest lucastrine sediments of Hamon) having the lowest share.