中文摘要：

为了试验3维反射地震方法在活断层探测中的应用效果,采用8线10炮的束状观测系统在银川盆地进行浅层3维反射地震试验,得到了反映芦花台断层3维空间结构的数据体。精细处理和综合解释的结果显示,芦花台断层由2条相向倾斜的隐伏正断层组成,主断层倾向SE,次断层倾向NW,二者在平面上的距离由北向南逐渐加大,在深度780~800m次断层归并到主断层上。主断层的上断点埋深自北向南逐渐加深,在试验区的北部上断点埋深为25~30m,而在试验区的南部上断点埋深为35~40m。试验结果表明,3维地震资料具有数据量大、信息丰富、偏移归位准确和断层成像精度高的特点,可以从不同方面反映地层、断层的3维空间展布形态,有利于复杂构造和断层的成像。

英文摘要：

To test the effect of three-dimensional seismic reflection methods used in active fault survey, we have done a three-dimensional shallow seismic reflection exploration experiment around the Luhuatai Fault in the west of Yinchuan Basin. The experiment uses swath geometry of 8 lines and 10 shots. Every two adjacent swaths overlap 3 survey lines, thus 5 swaths and 28 survey lines are laid in total. The ground sampling grid is 5m×20m and the CMP grid is 2.5m×5m. The data volume that reflects the three-dimensional spatial structure of the Luhuatai Fault is obtained. In data processing, we select the suitable three-dimensional seismic data process modules. The main processes are composed of raw data input, three-dimensional geometry defining and checking, anomalous trace edit and first arrival mute, spherical divergence compensation, surgical filtering to eliminate surface waves, surface-consistent amplitude compensation, surface-consistent deconvolution, velocity analysis and residual static correction（twice iteration）, DMO and the third time velocity analysis, final stacking, three- dimensional post-stack de-noising and horizontally interpolating, one-pass 3-D migration. 3-D seismic data interpretation uses the way of human-computer interaction. Through a variety of methods such as multi-line profiles contrasting, time slicing, three-dimensional visualization, and 3-D coherence cube technology, the reflection horizons are discerned and tracked, and the three-dimensional data volume reflecting the spatial variation of strata and faults is obtained. The results after fine processing and synthetical interpretation show that the Luhuatai Fault consists of two normal faults that incline to each other. The major fault inclines to SE, and the minor fault inclines to NW. The distance between them gradually increases from north to south. In addition, the minor fault merges into the major fault at the depth of approximately 780 ~ 800m. The up-breakpoint of the major fault has a tendency of deepening from north to south