Layered and blocked homogeneous models are usually used to calculated travel times and ray paths of wide-angle reflection waves in interpreting wide-angle reflection data of deep seismic sounding. 在研究地壳结构的人工源宽角反射地震资料解释中,常规宽角反射波走时和射线路径计算大都假定地壳模型为层状块状均匀介质。
By conventional seismotectonic interpretation, log interpretation and interwell stratigraphic correlation, I have finished geologic model building, which takes layered homogeneous medium model based on shortest path ray tracing theory. 通过常规地震构造解释、测井解释与井间地层对比,完成了地层模型的建立,采取以最短路径射线追踪理论为基础的层状均匀介质模型。