近十年来，深地震反射波勘探在海洋岩石圈的形成与演化、地壳结构研究中的应用越来越广泛。
In the recent decade, the deep seismic reflection profiling has been applied widely to studies on formation and evolution of oceanic lithosphere, crust structures and so on.
深地震反射剖面数据子库（简称SB1），系国土资源部深部地球物理探测数据库下属子库之一。
The Sub Database of Deep Seismic Reflection Profiling (called SB1 for short) is one of the seven sub databases under the Deep Geophysical Probing Database of the Ministry of Land and Resources.
随后英、法、德、加拿大和澳大利亚等国家相继开展了深地震反射研究计划，获得了岩石圈的形成与演化、地球深部构造等方面的重要信息。
Subsequently Britain, France, Germany, Canada, Australia developed deep seismic reflection research, and obtained lots of important information about form, development and deep structure.
深反射地震方法分辨率高、准确可靠，是用于地学研究的一种有效方法技术。
Deep reflection seismic method is characterized by high resolution ratio, accuracy and reliability, and is hence an effective technique for geoscience research.
此文介绍了在喜马拉雅山区进行的第一次深反射地震试验的结果。
Here we report the results of our first deep seismic reflection survey in Himalayan mountain country.
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.
本文通过虚反射机理分析，提出了充分利用虚反射能量设计最佳激发井深、增强下传地震波能量的采集方法。
Analyzing ghost mechanism, the paper presented the acquisition method fully using ghost energy to design the optimum shooting depth and strengthen the energy of down-propagating seismic waves.
该方法根据深反射地震技术的特点，从反射结构与能量的角度，突出深部构造。
According to characters of deep reflected seismic technology and starting from the Angle of reflected structure and energy, the method emphasized the deep structures.
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.
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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