Salt structures are important for several reasons, for example, due to its plastic properties, as well as its low and relatively constant density, salt can create intrusive structures such as diapirs, which can be studied and investigated in geological. In addition, considering the importance and increasing need for natural resources, including oil and gas, as well as the need for optimal storage of these resources and their use when it is necessary, identifying the structures and reservoirs that play a significant role in maintaining these resources, is important. Salt diapirs are among the geological structures that can store these resources due to their unique structure and characteristics. Geological evidence and geophysical data of the reflection seismic type, it is possible to provide a clear picture with details of the roof and floor surfaces of the salt structure as well as the sedimentary sequences and bedrock formations around it. Due to several reasons such as multiple reflections, wave polarization conversion, and energy loss reflected from steep salt surfaces, these data may not be able to provide enough details to interpret the salt mass and its surrounding structures. Therefore, by using seismic attributes such as gray level co-occurrence matrix, cosine of phase, instantaneous frequency, and also envelope, it can be used in the separation of salt from other layers and interpreted in the seismic section.