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.
目前世界震方法研究壳结构,通常借助于广角反射或折射,即震壳测方法,研究对象主要是莫霍面及其覆层的粗略结构。
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.
目前世界震方法研究壳结构,通常借助于广角反射或折射,即震壳测方法,研究对象主要是莫霍面及其覆层的粗略结构。
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