A New Method to Remove the Moveout of Azimuth Anisotropy Based on Difference

The paper introduces the difference method to analyze and remove the azimuth moveout resulted from anisotropy due to that correlation delay times varying with azimuth satisfy the hypothesis of the difference method. According to the testing from the pertinent example seismic data from a radial acquisition geometry based on an EDA media, the new method proposed is valid and implemented simply.