Analysis of potential field data in the wavelet domain

Various Green’s functions occurring in Poisson potential field theory can be used to construct non-orthogonal, non-compact, continuous wavelets. Such a construction leads to relations between the horizontal derivatives of geophysical field measurements at all heights, and the wavelet transform of the zero height field. The resulting theory lends itself to a number of applications in the processing of potential field data. Some simple, synthetic examples in two dimensions illustrate one inversion approach based upon the maxima of the wavelet transform (multiscale edges). These examples are presented to illustrate, by way of explicit demonstration, the information content of the multiscale edges. We do not suggest that the methods used in these examples be taken literally as a practical algorithm or inversion technique. Rather, we feel that the real thrust of the method is towards physically based, spatially local filtering of geophysical data images using Green’s function wavelets, or compact approximations thereto. To illustrate our first steps in this direction, we present some preliminary results of a 3-D analysis of an aeromagnetic survey.

[1]  G. M.,et al.  Partial Differential Equations I , 2023, Applied Mathematical Sciences.

[2]  A. S. Eve APPLIED GEOPHYSICS. , 1928, Science.

[3]  W. D. Evans,et al.  PARTIAL DIFFERENTIAL EQUATIONS , 1941 .

[4]  H. Fédérer Geometric Measure Theory , 1969 .

[5]  M. Al-Chalabi,et al.  SOME STUDIES RELATING TO NONUNIQUENESS IN GRAVITY AND MAGNETIC INVERSE PROBLEMS , 1971 .

[6]  D. Teskey,et al.  A system for rapid digital aeromagnetic interpretation , 1970 .

[7]  H. Naudy AUTOMATIC DETERMINATION OF DEPTH ON AEROMAGNETIC PROFILES , 1971 .

[8]  D. T. Thompson,et al.  EULDPH: A new technique for making computer-assisted depth estimates from magnetic data , 1982 .

[9]  A Stripping Filter For Potential-field Data , 1985 .

[10]  J. C. Mareschal Inversion of potential field data in Fourier transform domain , 1985 .

[11]  Robert W. Simpson,et al.  Approximating edges of source bodies from magnetic or gravity anomalies , 1986 .

[12]  Alan L. Yuille,et al.  Scaling Theorems for Zero Crossings , 1987, IEEE Transactions on Pattern Analysis and Machine Intelligence.

[13]  B. Jacobsen A case for upward continuation as a standard separation filter for potential-field maps , 1987 .

[14]  Lindrith Cordell,et al.  Limitations of determining density or magnetic boundaries from the horizontal gradient of gravity or pseudogravity data , 1987 .

[15]  Robert Hummel,et al.  Reconstructions from zero crossings in scale space , 1989, IEEE Trans. Acoust. Speech Signal Process..

[16]  Kenneth R. Piech,et al.  Fingerprints and fractal terrain , 1990 .

[17]  P. Tchamitchian,et al.  Regularite locale de la fonction “non-differentiable” de Riemann , 1990 .

[18]  Stéphane Mallat,et al.  Zero-crossings of a wavelet transform , 1991, IEEE Trans. Inf. Theory.

[19]  Stéphane Mallat,et al.  Characterization of Signals from Multiscale Edges , 2011, IEEE Trans. Pattern Anal. Mach. Intell..

[20]  Stéphane Mallat,et al.  Characterization of Self-Similar Multifractals with Wavelet Maxima , 1994 .

[21]  Gerald Kaiser,et al.  A Friendly Guide to Wavelets , 1994 .

[22]  R. Blakely Potential theory in gravity and magnetic applications , 1996 .

[23]  Richard J. Blakely Potential Theory in Gravity and Magnetic Applications: The Potential , 1995 .

[24]  F. Boschetti,et al.  Inversion of seismic refraction data using genetic algorithms , 1996 .

[25]  Matthias Holschneider,et al.  Wavelet analysis of potential fields , 1997 .

[26]  Stéphane Jaffard,et al.  Multifractal formalism for functions part I: results valid for all functions , 1997 .