摘要
地震转换波法是探测地壳与上地幔构造的方法之一.在辽宁选取两条近垂直的测线,收集了有关台站资料并用转换波法进行了解释,获得了一些有意义的深部数据.
Seismic converted wave is one of methods of explorating earth crust and upper mantle.In this paper,two measuring lines nearly vertical each other in Liaoning province are selected,and the data from relative stations are collected and explained with the method of seismic converted wave.So significant information of deep crustal structure is gotten.
引文
[1] 北京大学地球物理系教研室地震组,辽宁省地震局地震一队.辽宁南部地壳结构特征[J].北京大学学报(自然科学版),1978,(3):40—52.
[2] 邵学钟,张家茹,陈学华,等.京津唐地区地震转换波测深结果[J].地震地质,1980,2(2):11—20.