Abstract:Shear wave splitting,a key method for studying seismic anisotropy,is widely applied in seismic research. Different shear wave phases carry anisotropic information from various depths within the Earth. By analyzing shear wave splitting,the anisotropic characteristics of the medium can be inferred. This article provides a systematic introduction to the theoretical foundation of shear wave splitting,along with analysis methods for both local and distant earthquakes. It reviews recent advances in using shear wave splitting to investigate crustal stress fields in seismic source regions,seismic stress monitoring,deep Earth structures,and other related areas. The article also discusses future directions for the application of this method in geoscience. Through this review,readers will gain a comprehensive understanding of shear wave splitting and its significant applications in geoscience,providing valuable insights and guidance for further studies of seismic anisotropy.