3-DIMENSIONAL ELECTROMAGNETIC MODELING USING FINITE-DIFFERENCE EQUATIONS - THE MAGNETOTELLURIC EXAMPLE

被引:288
作者
MACKIE, RL [1 ]
SMITH, JT [1 ]
MADDEN, TR [1 ]
机构
[1] UNIV CAMBRIDGE,DEPT EARTH SCI,INST THEORET GEOPHYS,CAMBRIDGE CB2 3EQ,ENGLAND
关键词
D O I
10.1029/94RS00326
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We have developed a robust and efficient finite difference algorithm for computing the magnetotelluric response of general three-dimensional (3-D) models using the minimum residual relaxation method. The difference equations that we solve are second order in H and are derived from the integral forms of Maxwell's equations on a staggered grid. The boundary H field values are obtained from two-dimensional transverse magnetic mode calculations for the vertical planes in the 3-D model. An incomplete Cholesky decomposition of the diagonal subblocks of the coefficient matrix is used as a preconditioner, and corrections are made to the H fields every few iterations to ensure there are no H divergences in the solution. For a plane wave source field, this algorithm reduces the errors in the H field for simple 3-D models to around the 0.01% level compared to their fully converged values in a modest number of iterations, taking only a few minutes of computation time on our desktop workstation. The E fields can then be determined from discretized versions of the curl of H equations.
引用
收藏
页码:923 / 935
页数:13
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