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;
深反射地震资料处理的关键是从干扰背景中提取和增强深层弱有效信号，提高剖面的信噪比和分辨率。
The present paper has dealt systematically with a practical and effective deep reflection seismic technique—small-scale wide line reflection seismic technique.
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