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在解释辽南地区的闾阳—海城—东沟深地震测深剖面资料过程中,遇到了很多的,带有重要浅层速度信息的单支迴折波走时曲线。本文针对资料解释过程中出现的具体问题,提出了单支迴折波走时曲线解释的原理与方法,并且在 TI—59型计算机上得以实现。给出了相应的流程框图及计算机源程序,并且把此方法用于间阳—海城—东沟深地震测深剖面的资料解释中。获得了重要的浅层信息,并为该剖面的二维计算机处理提供了重要的参数。
During the interpretation of the Luyang-Haicheng-Donggou deep seismic sounding profile data in southern Liaoning Province, many single-stage buckling wave travel curves with important shallow velocity information were encountered. In this paper, in view of the specific problems that arise in the data interpretation process, the principle and method of explaining the travel time curve of single return wave are proposed and implemented on the TI-59 computer. The corresponding flow chart and computer source program are given, and the method is applied to the data interpretation of the deep-sea sounding profile of Xianyang-Haicheng-Donggou. Obtained important shallow information and provided important parameters for the 2D computer processing of the profile.