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ran is located in arid belt of the earth that the effect of the wind erosion is one of the main phenomena in this area. In global scale, it can be said that the risk and importance of wind erosion would not be less than water erosion. Sand dunes are the common and dominant shapes in these regions. So far, detailed geochemical analysis of these dunes, e.g. barchanoids, has not been carried out in Iran; thus, research on this subject can answer to fundamental questions about the geochemistry of these sand dunes in this area of Iran. Therefore, totally 27 sand dunes within 4 different zones were sampled and studied in this research that geographically coordinates N33° 28´ to 33° 34´ latitude and E58° 21´ to 58° 22´ longitude which are located in 13 Km south of Seh-Qaleh, Sarayan city in east of Iran that is a part of northern Lut Block and is greatly affected by wind erosion due to the climatic condition, several droughts, wind blow and lack of vegetation. For this purpose, firstly mineralogical compositions of Sarayan sand dunes have been studied by Rooney and Basu (1994) method and then 12 samples were collected and analyzed using XRF method for geochemical investigations. The mineralogical study in sand dunes of Sarayan indicates that the rock fragments has the highest frequency with 50 to 62 percent abundance (mean 60.11 percent), then quartz with 33 to 46 percent (mean 36.62 percent) and finally feldspar has 1 to 5 percent (with an average of 3.14 percent) abundance. Study on major oxides shows that the SiO₂ with 64.20 percent is mostly frequent oxide in comparison with the other major oxides of the studied samples. The resultant data of different oxides and relevant diagrams indicate an igneous, intermediate to felsic origin with normal quartz content and tectonically an active continental margin environment for Sarayan sand dunes. Calculated chemical index of Weathering (CIW) ranges between 82.81 to 84.96 percent which indicates an arid and warm climate. Also, slight chemical weathering and strong physical weathering in this region were approved. The study of heavy minerals can provide some evidences for recognition of probable source of sediments. Also, the values of major oxides such as MgO, Fe₂O₃ and TiO₂ can provide evidence of abundance or lack of heavy minerals. For this reason, firstly the amounts of Fe₂O₃, TiO₂ and MgO major oxides in 12 samples of sand dunes from four zones in a north-south direction were analyzed and no remarkable trend were found. Then the values of these major oxides in samples from four zones within a west-east direction were examined and revealed an east-ward decreasing trend. This issue related to northwestern winds that have a significant erosional influence and is in agreement with the direction of main northwestern wind which is responsible for the formation of barchanoid sand dunes in this region. The analysis of major oxides indicates that SiO₂ and Al₂O₃ are the most abundant oxides in the studied samples. The Al₂O₃ values plotted versus Na₂O and SiO₂ show a positive relationship whereas Al₂O₃ versus the other major oxides such as Fe₂O₃, K₂O, MgO, TiO₂ and MnO reveal negative trend that it can be related to lack of notable amounts of clay minerals and feldspar within the studied samples. On the other hand, positive relationship of Al₂O₃ and NaO₂ might be caused due to the presence of Na within the structure of alumino-silicate minerals. Moreover, the values of TiO₂ in the studied samples indicate a felsic to intermediate composition for source rock. The study of most important trace elements in the studied sand dunes showed high values of barium and zircon and also low amount of strontium which could be caused by frequency of original minerals such as K-feldspar and also deficiency of plagioclase within the source rocks. The low values of Sr might be related to negligible amounts of carbonate minerals, e.g. calcite and dolomite, within the studied samples. In addition, the amounts of trace elements such as Ba and Zr suggest a granitic and/or reworked sedimentary source rocks, associated with high concentration of heavy minerals. Furthermore, the application of weathering indices and graphs showed that plagioclase are slightly weathered and also weathering determination graphs suggest a negligible effect of chemical weathering in this area. Consequently, the main type of weathering in Sarayan region could be considered as physical weathering.