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远震层析成像中的地壳校正研究及应用
引用本文:江国明,赵大鹏,张贵宾.远震层析成像中的地壳校正研究及应用[J].地球物理学报,2009,52(6):1508-1514.
作者姓名:江国明  赵大鹏  张贵宾
作者单位:1.中国地质大学(北京)地球物理与信息技术学院,北京 100083;2.日本东北大学地球物理系,仙台 980-8578
基金项目:863计划重大项目,日本文部科学省研究基金 
摘    要:远震层析成像是研究一个地区上地幔三维速度结构的有力手段.但由于远震射线在地壳内的交叉较差,因此无法准确约束地壳内的三维速度结构.为了消除地壳内横向不均匀性对深部速度成像产生的影响,必须进行地壳校正.本文详细描述了地壳校正的基本原理和步骤,主要包括三维地壳模型的选取、地壳内走时差的计算以及校正后的相对走时差的计算.以勘察加地区为例,通过计算各台站的平均相对走时差和远震层析成像结果分析了地壳校正的实际效果,同时验证了该方法的实用性.

关 键 词:地壳校正  远震层析成像  走时差  三维地壳模型  
收稿时间:2008-9-16
修稿时间:2008-11-20

Crustal correction in teleseismic tomography and its application
JIANG Guo-Ming,ZHAO Da-Peng,ZHANG Gui-Bin.Crustal correction in teleseismic tomography and its application[J].Chinese Journal of Geophysics,2009,52(6):1508-1514.
Authors:JIANG Guo-Ming  ZHAO Da-Peng  ZHANG Gui-Bin
Institution:1.School of Geophysics and Information Technology, China University of Geosciences (Beijing), Beijing 100083, China;2.Department of Geophysics, Tohoku University, Sendai 980-8578, Japan
Abstract:Teleseismic tomography is a powerful technique for determining the 3-D upper mantle structure under a region, but it cannot determine the 3-D crustal structure well because the teleseismic rays do not crisscross well in the crust. Hence it is crucial to make crustal corrections to remove the effect of lateral crustal heterogeneity from the observed travel-time data. In this work we describe a technique for conducting the crustal correction in teleseismic tomography, which includes the choice of 3-D crustal model, the calculations of the travel-time residual in the crust and the relative residual after the crustal correction. We choose the Kamchatka region as an experiment to analyze the validity of the crustal correction via the mean relative residuals at each station and the results of teleseismic tomography, and also to verify the applicability of the technique for making crustal correction.
Keywords:Crustal correction  Teleseismic tomography  Travel-time residual  3-D crustal model
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