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.
出处
《西北地震学报》
CSCD
北大核心
2003年第2期149-154,共6页
Northwestern Seismological Journal
关键词
地震转换波
辽宁
深部构造
Seismic converted wave
Liaoning
Deep structure
