在深部地质调查中,深反射地震剖面发挥了重要作用。
The deep reflection seismic profile plays an important role in deep geological survey.
深反射地震剖面的解释要着眼于大的地质构造运动和成因,运用地质规律进行综合地质解释。
The interpretation of the deep reflection seismic profile should be focused on the large geological tectonism and its genesis;
因而,在常规的地震剖面上,来自河道砂岩体上的反射是不易识别的。
So it is often difficult to identify the reflections from the channel sand body on conventional seismic sections.
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