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基于分区多步快速行进法下3D起伏层状介质中多震相射线追踪
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  • 英文篇名:Multi-phase seismic ray tracing in 3D undulated layered media based on multistage FMM algorithm
  • 作者:张云 ; 严星 ; 白超英
  • 英文作者:ZHANG Yun;YAN Xing;BAI Chao-ying;Department of Geophysics,School of Geology Engineering and Geomatics,Chang'an University;Xinjiang University of Finance and Economic;Institute of Computational Geophysics,Chang'an University;
  • 关键词:快速行进法(FMM) ; 不规则最短路径法(ISPM) ; 分区多步计算技术 ; 不等距上行差分格式 ; 上行有限差分算法 ; 多震相射线追踪
  • 英文关键词:Fast Marching Method(FMM);;Irregular Shortest-Path Method(ISPM);;multistage computational technique;;uneven grid upwind differential format;;upwind finite-difference method;;multiphase seismic ray tracing
  • 中文刊名:DQWJ
  • 英文刊名:Progress in Geophysics
  • 机构:长安大学地质工程与测绘学院地球物理系;新疆财经大学网络与实验教学中心;长安大学计算地球物理研究所;
  • 出版日期:2018-01-24 09:15
  • 出版单位:地球物理学进展
  • 年:2018
  • 期:v.33;No.149
  • 语种:中文;
  • 页:DQWJ201803016
  • 页数:9
  • CN:03
  • ISSN:11-2982/P
  • 分类号:111-119
摘要
快速行进法(FMM)是一种求解程函方程数值解计算网格节点走时,然后向后处理进行射线追踪的方法.为了求取任意起伏界面下高精度多震相的地震走时与相应的射线路径,本文采用任意起伏地表条件下的的三维不等距上行差分公式结合分区多步计算技术实现了三维复杂层状起伏介质中多震相(透射、反射、转换波)地震走时的计算,利用上行有限差分公式逐次进行射线路径的追踪,并且通过与较为成熟的不规则最短路径法(ISPM)对比,验证了本算法的计算精度和有效性.数值模拟实例和对比结果表明该算法具有较高的计算精度,数值计算稳健,能灵活处理含任意三维起伏界面模型中多震相地震走时及相应射线路径的追踪问题.
        Fast Marching Method(FMM) for ray tracing is a method using numerical solutions of Eikonal equation to calculate the traveltime of all gridded points, and applying backward processing ray tracing for obtaining raypath information. To obtain a high accurate traveltimes in 3D complex media with undulated topography,we in this paper calculate the traveltime and tracking arrivals composed of any kind of combinations of transmissions,conversions and reflections by integrating upwind finite difference method and multistage computation technique in complex 3D complex media. In addition, the accuracy and efficiency of proposed algorithm are compared with the well developed Irregular Shortest-path Method(ISPM). We use an uneven differential format to compute the traveltimes at the irregular grids near the subsurface interface, and establish a upwind finite-difference formula for tracking raypaths. Finally,the traveltime computation and the corresponding raypaths finding for multi-phase arrivals are solved flexibly by multistage computation technique. The simulation and comparison tests show that the proposed algorithm has a high computational accuracy,numerical stability and flexible adaptability in traveltime computation and raypath finding for multi-phase seismic arrivals in any 3D complex media.
引文
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