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本文所介绍的,系与断层有关的特殊波之一,全文共分绕射、断面反射两部分。完全基于运动地震学,没有进行动力学方面的探讨。叙述了它们产生的机理、特征及其公式;剩余时差及其对迭加效果的探讨;最后利用初步研究的成果,结合苏北地区部分实际资料,依据绕射波极小点座标和断面反射的实际构组,较为可靠地确定了该区几条断层。
This paper introduces one of the special faults related to faults, the full text is divided into two parts: diffraction and cross section. Based entirely on kinematic seismology, no kinetic studies have been conducted. Describes the mechanism, characteristics and formulas of their generation; the remaining time difference and its discussion of the superposition effect; finally, based on the results of the preliminary study and some actual data in North Jiangsu, based on the coordinates of the minimum point of the diffraction wave and the reflection of the section The actual formation, more reliable to determine the area several faults.