1887
2nd Australasian Exploration Geoscience Conference: Data to Discovery
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

The magnetotelluric method has been successfully used as a complementary tool in the exploration of foothill plays but its intrinsic non-uniqueness and its reduced structural fidelity, with respect to a seismic section, make its interpretation more complex.

Since the solution of a non-unique inverse problem is heavily dependent on its starting point, a traditional method to tackle the non-uniqueness relies on the careful definition of the starting model, used as a tool for injecting the available a-priori information into the inverse problem.

We present an alternative approach to the exploitation of the a-priori knowledge that, instead of embedding it into the starting model, relies on the continuous assimilation of the structural/geological information into the resistivity volume. The method we propose for the inversion of the MT soundings tries to maximize, simultaneously, the data-fit and the structural fidelity. We discuss the advantages deriving from the application of this technique by mean of a synthetic example representative of a foothills play.

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/content/journals/10.1080/22020586.2019.12073124
2019-12-01
2026-01-23
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References

  1. Constable, S., Orange, A., and Key, K. [2015] And the geophysicist replied: “Which model do you want?”. Geophysics, 80(3), E197-E212.
  2. De Stefano, M., Golfré Andreasi, F., Re, S., Virgilio, M., and Snyder, F. F. [2011]. Multiple-domain, simultaneous joint inversion of geophysical data with application to subsalt imaging. Geophysics, 76(3), R69-R80.
  3. Farquharson, C.G. and Craven, J.A. [2009]. Three-dimensional inversion of magnetotelluric data for mineral exploration: An example from the McArthur River uranium deposit, Saskatchewan, Canada. Journal of Applied Geophysics, 68(4), 450-458.
  4. Gallardo, L. A., and Meju, M. A. [2007]. Joint two-dimensional cross-gradient imaging of magnetotelluric and seismic traveltime data for structural and lithological classification. Geophysical Journal International, 169(3), 1261-1272.
  5. Golfré Andreasi, F. and Masnaghetti, L. [2015]. Decoupled Model Grids for Simultaneous Joint Inversion of MT and CSEM Data. 77th EAGE Conference and Exhibition Extended Abstracts, N105.
  6. Golfré Andreasi, F., Re, S., Ceci, F. Masnaghetti, L. and Battaglini A., [2018] Geologically-Driven Inversion of Magnetotelluric Data. 2nd Conference on Geophysics for Mineral Exploration and Mining, Extended Abstract
  7. Hui, C., Deng, J. and Yin, C. [2016]. Three-dimensional electrical structures of Jiurui ore district in the middle-lower Yangtze River Metallogenic Belt, eastern China from AMT inversion. 86th SEG International Exposition and Annual Meeting, Extended Abstracts.
  8. McIntosh, S., [2009]. The role of geophysics in mineral deposit discovery: a Rio Tinto perspective. Preview, 139, 39-46.
  9. Tartaras, E., Masnaghetti, L., Lovatini, A., Hallinan, S., Mantovani, M., Virgilio, M., Soyer, W., De Stefano, M., Snyder, F., Subia, J. And Dugoujard, T. [2011] Multi-property earth model building through data integration for improved subsurface imaging. First Break, 29(4), 83-88.
  10. Zerilli, A., Lovatini, A., Battaglini, A. and Menezes, P.D.L. [2012] Resolving Complex Overthrust Features Using Magnetotellurics – The Bolivian Foothills Case Study. First EAGE/ACGGP Latin American Geophysics Workshop.
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  • Article Type: Research Article
Keyword(s): geology; inversion; magnetotellurics; structural
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