<%@LANGUAGE="JAVASCRIPT" CODEPAGE="1252"%> Geophysics
Fabio Boschetti,
Research Scientist,
CSIRO CMAR, Australia
Publications
Complex System Science
Ecological Modelling
Can we learn how systems work?
Agent Based, Economic Modelling & Game Theory
Emergence
Modelling the non-separability of a very complex world (ECCS'10)
Optimisation
Visualisation of scientific data
Geophysics
CV
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Geophysics

This is my past life, so all this work is now dated. It covers mostly image processing and inversion

 

Image Processing

Multiscale analysis of geophysical images

We developed a mathematical framework which allows for the analysis, processing and inversion of gravity and magnetic images, based on multiscale edges. These edges represent the main features in an image, and they are a significant aid in the visual analysis and interpretation of potential field images. Also, under restrictive but geologically reasonable assumptions, these edges have simple spatial relationships with the location of contacts between bodies of different density and/or susceptibility and can consequently be used in an inverse process to reconstruct approximate 3-D models of the underground geology

  • F. Boschetti, P. Hornby and F.G. Horowitz, 2001, Wavelet based inversion of gravity data, Exploration Geophysics, 32, 48-55.
  • D. Holden, N. Archibald, F. Boschetti, M. Jessell, 2001, "Inferring Geological Structures Using Wavelet-Based Multiscale Edge Analysis and Forward Models", Exploration Geophysics.
  • Hornby, P., F. Boschetti, and F.G. Horowitz, "Analysis of Potential Field Data in the Wavelet Domain", Geophysical Journal International, 137, 175-196, 1999.
  • Archibald, N.J., P. Gow, and F. Boschetti, Multiscale edge analysis of potential field data, 1998, Exploration Geophysics., 30, 38-44.
  • Feature removal and improved downward continuation of potential field maps

    Building on the theory developed in the multiscale analysis of geophysical images, we are able to isolate or remove individual anomalies from potential field maps. Depending on the purpose of the processing, we can either leave adjacent anomalies untouched, or account for the effects of the removed anomaly. Also, by constraining the process with the information contained in the multiscale edges, improvement in the sharpening inherent in the downward continuation of potential field maps can be achieved, thereby considerably improving the visual inspection of gravity and magnetic signals

    Other Geophysical Signal processing

    Inversion of geophysical data

    Boschetti, F., Therond, V., and Hornby, P., 2004, Feature removal and isolation in potential field data, Geophysical Journal International, Volume 159 Issue 3 Page 833.;