3D velocity modeling for mineral exploration via ambient noise tomography

ABSTRACT An application of ambient noise tomography (ANT) for mineral exploration near the town of Marathon, Ontario, Canada, is documented. The study area consists of host rocks for platinum group metals and copper. ANT was performed to generate a 3D shear-wave velocity (VS) model for the exploration of Marathon deposits. The ambient noise recordings used were collected using 90 vertical geophones for 26 days. The recordings were used to compute the noise correlation functions and estimate Rayleigh wave phase and group velocity dispersion curves. Then, these dispersion measurements were used for 2D tomography to create 2D velocity maps that were inverted to obtain a 3D VS model. The independently produced VS model shows good agreement with the measured VS from downhole VS logging. Furthermore, the developed 3D velocity model aids in interpretation of the study area that can be helpful for future mineral exploration and for improving understanding of the mineral generation model.

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Publication Details

Journal
Geophysics
Published
2025-10-27
DOI
https://doi.org/10.1190/geo-2024-0958
Primary Topic
Seismic Imaging and Inversion Techniques
Type
article
Field-Weighted Citation Impact
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3D velocity modeling for mineral exploration via ambient noise tomography

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3D velocity modeling for mineral exploration via ambient noise tomography

Sheri Molnar, Nicholas Arndt, Adebayo Oluwaseun Ojo, David Good, Chanelle Boucher, Michael C. Pitts, John H. McBride, Hema Sharma, Dan Hollis, Charles D. Beard
article en

Abstract

ABSTRACT An application of ambient noise tomography (ANT) for mineral exploration near the town of Marathon, Ontario, Canada, is documented. The study area consists of host rocks for platinum group metals and copper. ANT was performed to generate a 3D shear-wave velocity (VS) model for the exploration of Marathon deposits. The ambient noise recordings used were collected using 90 vertical geophones for 26 days. The recordings were used to compute the noise correlation functions and estimate Rayleigh wave phase and group velocity dispersion curves. Then, these dispersion measurements were used for 2D tomography to create 2D velocity maps that were inverted to obtain a 3D VS model. The independently produced VS model shows good agreement with the measured VS from downhole VS logging. Furthermore, the developed 3D velocity model aids in interpretation of the study area that can be helpful for future mineral exploration and for improving understanding of the mineral generation model.

GeophysicsVol. 91(1)
Barrick Gold (Canada) (CA), Western University (CA), University of Applied Sciences Utrecht (NL), Golder Associates (Canada) (CA), Utrecht University (NL), Institut des Sciences de la Terre (FR), Systématique, adaptation, évolution (FR), Université Gustave Eiffel (FR), Université Grenoble Alpes (FR), Ontario Power Generation (CA)
Openalex Percentile: Top 67%
Seismic Imaging and Inversion Techniques
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