Improved methods for solving for the magnetic field in E-polarization induction problems with fixed and staggered grids
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/126/2/437/5917076/126-2-437.pdf
Reference13 articles.
1. One- and two-dimensional inversion of magnetotelluric data in continental regions;Agarwal;Phys. Earth planet. Inter.,1993
2. On the firms difference solution of two-dimensional induction problems;Brewitt-Taylor;Geophys. J. R. astr. Soc.,1576
3. Three-dimensional magnetotelluric modeling using difference equations-Theory and comparisons to integral equation solutions;Mackie;Geophysics,1993
4. Three-dimensional electromagnetic modeling using finite difference equations: The magnetotelluric example;Mackie;Radio Science,1994
5. Madden, T.R. , 1972. Transmission systems and network analogies to geophysical forward and inverse problems, ONR Tech Rep., 72-73.
Cited by 3 articles. 订阅此论文施引文献 订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献
1. COMPARISON OF FINITE DIFFERENCE NUMERICAL SOLUTIONS IN MAGNETOTELLURIC MODELLING;CHINESE J GEOPHYS-CH;2010
2. EM2INV — A finite difference based algorithm for two-dimensional inversion of geoelectromagnetic data;Journal of Earth System Science;1999-12
3. A hybridized mixed finite element domain decomposed method for two dimensional magnetotelluric modelling;Earth, Planets and Space;1999-04
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