近年来,由于地震勘探广泛采用了多次覆盖技术和现代计算技术,使地震勘探能力获得大幅度的提高,其地质找矿效果亦日益显著而被誉为地震技术发展史上的一次“革命”。因此,新技术方法所得之地震资料的地质效果,已由五十年代只能识别简单地质构造的几何形态,进而深化到可以精确的判定幅度小、构造复杂的地质现象,甚至还可以解释地层的岩性以及相关的沉积环境等等。 In recent years, due to the extensive coverage of seismic exploration technology and modern computing technology, the seismic exploration capability has been greatly improved, and its geological prospecting effect is also increasingly significant and known as a seismic technology in the history of a “revolution.” Therefore, the geological effects of the seismic data obtained by the new technique method have been limited only by recognizing the geometry of simple geological formations in the 1950s, and further deepening to accurately determine the geological phenomena with small amplitude and complicated structures. It is even possible to explain the geological Lithology and related sedimentary environment and so on.