1887
3D Electromagnetics
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

A major challenge in 3-D Magnetotelluric (MT) data inversion is the considerable computational resources required. Most efforts at 3-D MT inversion have been formulated directly in the model space, so that the size of all computations depends strongly on the value of the number of model space parameters. For geologically realistic 3-D models, can be quite large, and in particular is typically much larger than the total number of MT impedance data By transforming the inversion into the data space, the computational demands can be significantly decreased. In this paper, we present an Occam style 3-D inversion algorithm based on a data space formulation. Inversion results for synthetic data display good convergence. The data space method can also be used with other types of inversion algorithm such as data sub-space techniques. These refinements will allow more efficient and robust 3-D inversion algorithms to be developed.

Loading

Article metrics loading...

/content/journals/10.1071/ASEG2003_3DEMab017
2003-04-01
2026-01-21
Loading full text...

Full text loading...

References

  1. Constable, C. S., Parker, R. L., and Constable, C.G., 1987, Occam’s inversion: A practical algorithm for generating smooth models from electromagnetic sounding data, Geophysics, 52, 289-300.
  2. deGroot-Hedlin, C, and Constable, S., 1990, Occam’s inversion to generate smooth, two-dimensional models from magnetotelluric data, Geophysics, 55, 1613-1624.
  3. Egbert, G. D., Bennett, A. F., and Foreman, M. G, 1994, TOPEX/POSEIDON tides estimated using a global inverse model, Journal Geophysical Research, 99: 24821-24852.
  4. Mackie, R. L., and Madden, T. R., 1993, Three-dimensional magnetotelluric inversion using conjugate gradients, Geophysical Journal International, 115: 215-229.
  5. Mackie, R L., Smith, J. T., and Madden, T. R, 1994, Three-dimensional electromagnetic modeling using finite difference equations: The magnetotelluric example, Radio Science, 29: 923-935.
  6. Newman, G. A., and Alumbaugh, D. L., 2000, Three-dimensional magnetotelluric inversion using non-linear conjugate gradients, Geophysical Journal International, 140, 410-424.
  7. Parker, R. L., 1994, Geophysical Inverse Theory: Princeton University Press.
  8. Sasaki, Y., 2001, Full 3-D inversion of electromagnetic data on PC, J. Apply Geophysics, 46: 45-54.
  9. Siripunvaraporn, W., and Egbert, G, 2000, An Efficient Data-Subspace Inversion Method for 2-D Magnetotelluric Data, Geophysics, 65, 791-803.
  10. Siripunvaraporn, W., Egbert, G, and Lenbury, Y., 2002, Numerical accuracy of magnetotelluric modeling: A comparison of finite difference approximations, Earth Planets Space, 54, 721-725.
/content/journals/10.1071/ASEG2003_3DEMab017
Loading
  • Article Type: Research Article
Keyword(s): 3-D Inversion; Data-Space Method; Magnetotelluric; Occam’s Inversion,
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error