According to the amplitude of vibration,wave group continuity and forms of seismic waves reflected on the 6 sections,the Meso Cenozoic,Upper Paleozoic,Predevonian,Precambrian,intrusive mass and the basic magma basement could be identified.

• 利用深部地震剖面上反射波的振幅强弱、波组连续性和波组外形等识别标志 ,可识别出中、新生界、上古生界、前泥盆系、前寒武系、侵入岩体和基性岩浆底垫等地质体 ;