Gas hydrates are crystalline solids of water molecules that are linked together by hydrogen bonding. And there are gas molecules in the empty space available on this network. The presence of gas hydrates in an area influences the physical and seismic properties of host sediments. Seismic attributes are among the most suitable tools for seismic investigations. The first indication of the presence of gas hydrates in the seismic sections of the sea regions is the Bottom Simulating Reflector (BSR). In this study, first, BSR-related attributes have been identified, then the values of these attributes are obtained in areas including the BSR and the regions without BSR. Using principal component analysis (PCA) dimming algorithms, these values are based on the degree of importance of diminishing the dimension. In this study, the principal component analysis algorithm is able to provide a better separation than the initial attributes between the BSR and the regions without BSR.