Advances in three-dimensional magnetotelluric modeling using integral equations

Recent progress in integral equation modeling of three‐dimensional magnetotelluric responses includes the ability to simulate 3-D structures which outcrop (excluding topography), which transect layer interfaces, and which extend indefinitely in one or more directions. The most important factor in achieving this capability is an accurate treatment of the electric surface charge. In particular, a previous integro‐difference formulation for evaluating charges has been abandoned in favor of true surface integrations over the source cells with potential differencing across the field cells in the 3-D body. The new procedure constitutes a good approximation to Galerkin’s method while preserving internal consistency in terms of pulse basis functions. To verify outcropping structures, juxtaposed conductive and resistive prisms at the surface are simulated and compared to 2-D results. An elongate version of the 3-D model shows good agreement with both transverse electric and transverse magnetic modes of the 2-D res...

[1]  A. Ralston A first course in numerical analysis , 1965 .

[2]  O. D. Kellogg Foundations of potential theory , 1934 .

[3]  Gerald W. Hohmann,et al.  Magnetotelluric responses of three-dimensional bodies in layered earths , 1982 .

[4]  S. Constable,et al.  Occam's inversion to generate smooth, two-dimensional models from magnetotelluric data , 1990 .

[5]  G. W. Hohmann Three-Dimensional Induced Polarization and Electromagnetic Modeling , 1975 .

[6]  J. Van Bladel,et al.  Some remarks on green's dyadic for infinite space , 1961 .

[7]  Philip E. Wannamaker,et al.  A stable finite element solution for two-dimensional magnetotelluric modelling , 1987 .

[8]  R. Harrington Time-Harmonic Electromagnetic Fields , 1961 .

[9]  W Hohmann Gerald,et al.  Numerical modeling for electromagnetic methods of geophysics , 1987 .

[10]  Peter R. Bannister,et al.  Applications of complex image theory , 1986 .

[11]  G. W. Hohmann,et al.  The telluric‐magnetotelluric method in two‐ and three‐dimensional environments , 1981 .

[12]  Alan G. Jones,et al.  Resistivity cross section through the Juan de Fuca Subduction System and its tectonic implications , 1989 .

[13]  D. A. H. Jacobs,et al.  A Generalization of the Conjugate-Gradient Method to Solve Complex Systems , 1986 .

[14]  On thin‐layer telluric modeling of magnetotelluric responses , 1990 .

[15]  Walter L. Anderson,et al.  Computer program; numerical integration of related Hankel transforms of orders O and 1 by adaptive digital filtering , 1979 .

[16]  Gerald W. Hohmann,et al.  Integral equation solution for the transient electromagnetic response of a three-dimensional body in a conductive half-space , 1985 .

[17]  R. L. Mackie,et al.  Three-dimensional magnetotelluric modelling and inversion , 1989, Proc. IEEE.

[18]  John F. Hermance,et al.  The asymptotic response of three-dimensional basin offsets to magnetotelluric fields at long periods; the effects of current channeling , 1982 .

[19]  Gerald W. Hohmann,et al.  Electromagnetic modeling of three-dimensional bodies in layered earths using integral equations , 1983 .

[20]  Roger F. Harrington,et al.  Field computation by moment methods , 1968 .