得好地震反射标准波是提高地震勘探效果的重要措施、是查明断层和构造形态的技术关键。在反复研究新老地区地层结构并重新分析原有地震资料的础基上,使我们认识到该区客观存在着高速薄层这一事实,对薄层反射的可能性及其特点进行了认真研究,大量 Well received seismic reflection standard wave is an important measure to improve the seismic exploration effect and is the key to identify faults and tectonic forms. Repeatedly studying the stratigraphic structure of the old and new areas and reanalyzing the foundation of the original seismic data has led us to recognize the fact that there is an objective existence of high-speed thin layers in this area. The possibility and characteristics of thin-layer reflections have been carefully studied A lot