Geophysical inversion contributions to mineral exploration: lessons from the Footprints project
| Autor: | Richard S. Smith, Pejman Shamsipour, Kevin M. Ansdell, Julia J. King, Ken Wasyliuk, Colin G. Farquharson, Reza Mir, Michel Chouteau, Marc A. Vallée, William A. Morris, Robert G. Lee, Randolph J. Enkin, Stéphane Perrouty |
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| Rok vydání: | 2019 |
| Předmět: |
Geophysical inversion
Gravity (chemistry) 010504 meteorology & atmospheric sciences Potential field 3d model Geophysics 010502 geochemistry & geophysics 01 natural sciences Magnetic susceptibility Physics::Geophysics Mineral exploration General Earth and Planetary Sciences Geology 0105 earth and related environmental sciences |
| Zdroj: | Canadian Journal of Earth Sciences. 56:525-543 |
| ISSN: | 1480-3313 0008-4077 |
| Popis: | Magnetic and gravity inversions are used to create 2D or 3D models of the magnetic susceptibility and density, respectively, using potential field data. Unconstrained inversions generate an output based on mathematical constraints imposed by the inversion algorithm. Constrained inversions integrate lithological, structural, and petrophysical information in the inversion process to produce more geologically meaningful results. This study analyses the validity of this assertion in the context of the NSERC-CMIC Mineral Exploration Footprints project. Unconstrained and constrained geophysical inversions were computed for three mining sites: a gold site (Canadian Malartic, Québec), a copper site (Highland Valley, British Columbia), and a uranium site (Millennium – McArthur River, Saskatchewan). After initially computing unconstrained inversions, constrained inversions were developed using physical property measurements, which directly link geophysics to geology, and lithological boundaries extracted from an interpreted geological model. While each derived geological model is consistent with the geophysical data, each site exhibited some magnetic complexity that confounded the inversion. The gold site includes regions with a strong magnetic signature that masks the more weakly magnetic zone, thereby hiding the magnetic signature associated with the ore body. Initial unconstrained inversions for the copper site yielded solutions with invalid depth extent. A consistency between the constrained model and the geological model is reached with iterative changes to the depth extent of the model. At the uranium site, the observed magnetic signal is weak, but the inversion provided some insights that could be interpreted in terms of an already known complexly folded geological model. |
| Databáze: | OpenAIRE |
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