琼东北及雷州半岛深地震测深剖面Pg波资料处理结果——用地震波前成像和射线数分布分析法
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摘要
本文用地震波前成像和射线数分布分析法对上世纪80年代在琼东北及雷州半岛地区完成的三条宽角反射/折射地震剖面的Pg波资料进行了处理,得到了三条测线下方的上地顶部P波速度结构及基底的空间展布形态特征.结果显示研究区域表现出较复杂的上部地结构特征,浅部P波速度结构的高、低速区域分别与地质构造上的一些凸起和凹陷相对应,用射线数分布分析法所显示的基底结构及形态特征与地震剖面穿过区域的地质构造有较好的对应关系,测线穿过的一些断裂下方P波速度结构表现为强烈的横向非均匀性.
The Pg traveltimes picked from three wide-angle reflection/refraction profiles,which were completed at the beginning of the1980s in Northeast Hainan and Leizhou Peninsula area of South China,were used to reconstruct P velocity images and basement structures of uppermost crust by means of seismic wavefront tomography and ray hit analysis technique.Both P wave velocity structure and the spatial basement pattern of uppermost crust were determined,and the results were compared with the geological structures along the three profiles.It is found that the uppermost crustal structures in this area show relatively complex characteristics.The distribution of higher or lower P wave velocities in the uppermost crust corresponds to some geological depressions and raisings,respectively.It shows no more difference between the geological tectonic characteristics and the basement structures along with their pattern features obtained through ray hit analysis technique.The distribution of P wave velocities presents strong laterally inhomogeneity under the areas where the faults exist.
引文
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