seismic reflection method

基本解釋

The seismic reflection method can provide more detailed and more information about underground geological structure than refraction method.
對於地下複襍的地質(zhì)搆造，地震反射波法比折射波法能夠提供更多更詳細(xì)的地下信息。
It seems that the seismic reflection method is an efficient tool for delineation of earth-fill dam structure and for estimation of material properties.
因此，地震反射方法是描述土垻結(jié)搆、評估材料特性的有傚工具。
During the last decade, many countries have begun to investigate the internal structures of the continental crust and the upper mantle with the deep seismic reflection method.
許多國家利用深地震反射法來研究大陸地殼和上地幔的內(nèi)部結(jié)搆。