层状弹性介质全波射线追踪技术研究
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  • 英文篇名:Full-wave ray tracing technology research on layered elastic medium
  • 作者:孙明武 ; 孟凡顺 ; 王璐 ; 秦显科
  • 英文作者:SUN Ming-wu;MENG Fan-shun;WANG Lu;QIN Xian-ke;College of Marine Geo-science,Ocean University of China;
  • 关键词:全波射线追踪 ; 透射损失 ; 球面扩散 ; 转换波 ; 四叉树
  • 英文关键词:full-wave ray tracing;;transmission loss;;spherical diffusion;;converted wave;;quaternary tree
  • 中文刊名:DQWJ
  • 英文刊名:Progress in Geophysics
  • 机构:中国海洋大学海洋地球科学学院;
  • 出版日期:2017-02-15
  • 出版单位:地球物理学进展
  • 年:2017
  • 期:v.32;No.141
  • 语种:中文;
  • 页:DQWJ201701037
  • 页数:7
  • CN:01
  • ISSN:11-2982/P
  • 分类号:272-278
摘要
射线追踪法是一种有效的地震波场数值模拟方法,在层析成像、叠前深度偏移及正演模拟等研究领域均占据重要地位.但相较于波动方程数值模拟方法,射线追踪法在获取较高运算速度的同时损失掉了地震波场的动力学信息,对于整个地震波场的地震波衰减以及转换波等问题都没有进行考虑.为了能够得到较为完整的合成地震记录并对地震资料做出更合理解释,本文在使用射线追踪法进行波场数值模拟的同时考虑了衰减信息,追踪转换波以弥补射线追踪法在动力学上的缺陷.在全波射线追踪过程中,通过追踪同类波和转换波,并计算该段射线的能量衰减,在保证高速计算的同时获得了较为完整的合成地震记录,取得较好的效果.
        Ray-tracing method is an effective numerical simulation method ofseismic wave field,and occupies animportant position in tomography,pre-stack depth migration,forward modeling and other research areas. Compared with the wave equation numerical simulation method,ray tracing method is gettinga highercalculatingspeed,while losing the dynamic information of the seismic wave field,besides,the whole seismic wave field's problems of wave attenuation andconversionare not considered. In order to get a relatively complete synthetic seismogram and make more reasonable interpretation of seismic data,this paper usesray-tracing method to simulate the wave field,meanwhile,takesthe informationattenuation into account and tracesconverted wave to make up the defects of the ray-tracing methodon dynamics. In the process offull-wave ray tracing, by tracingsimilar wave and converted wave, and calculating theray energy attenuation, we obtain a relatively complete synthetic seismogram maintaining high calculating speed, which achieved favorable result.
引文
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