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.
目前世界上用方法结构,通常借助于广角反射或折射,即测方法,对象主要是莫霍面及其上覆层的粗略结构。
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.
目前世界上用方法结构,通常借助于广角反射或折射,即测方法,对象主要是莫霍面及其上覆层的粗略结构。
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