Nowadays the wide angle reflection/refraction-the deep-crustal sounding is usually used as a seismic method in the world mainly for Studying rough structure of Moho &its overling beds.
目前世界上用地震方法研究地壳结,借助于广角反射或折射,即地震地壳测方法,研究对象主要是莫霍面及其上覆略结。
Nowadays the wide angle reflection/refraction-the deep-crustal sounding is usually used as a seismic method in the world mainly for Studying rough structure of Moho &its overling beds.
目前世界上用地震方法研究地壳结,借助于广角反射或折射,即地震地壳测方法,研究对象主要是莫霍面及其上覆略结。
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