3-D geochemical interpolation guided by geophysical inversion models

3-D geochemical subsurface models, as constructed by spatial interpolation of drill-core assays, are valuable assets across multiple stages of the mineral industry's workflow. However, the accuracy of such models is limited by the spatial sparsity of the underlying drill-core, which samples onl...

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Main Authors: Tom Horrocks, Eun-Jung Holden, Daniel Wedge, Chris Wijns
Format: Article
Language:English
Published: Elsevier 2021-05-01
Series:Geoscience Frontiers
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674987120302218
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spelling doaj-efd07d75a8c84e55ac0ee9a455e4819a2021-04-04T04:18:36ZengElsevierGeoscience Frontiers1674-98712021-05-011231010893-D geochemical interpolation guided by geophysical inversion modelsTom Horrocks0Eun-Jung Holden1Daniel Wedge2Chris Wijns3Corresponding author.; Centre for Exploration Targeting. School of Earth Sciences, University of Western Australia, Crawley, WA 6009, AustraliaCentre for Exploration Targeting. School of Earth Sciences, University of Western Australia, Crawley, WA 6009, AustraliaCentre for Exploration Targeting. School of Earth Sciences, University of Western Australia, Crawley, WA 6009, AustraliaCentre for Exploration Targeting. School of Earth Sciences, University of Western Australia, Crawley, WA 6009, Australia3-D geochemical subsurface models, as constructed by spatial interpolation of drill-core assays, are valuable assets across multiple stages of the mineral industry's workflow. However, the accuracy of such models is limited by the spatial sparsity of the underlying drill-core, which samples only a small fraction of the subsurface. This limitation can be alleviated by integrating collocated 3-D models into the interpolation process, such as the 3-D rock property models produced by modern geophysical inversion procedures, provided that they are sufficiently resolved and correlated with the interpolation target. While standard machine learning algorithms are capable of predicting the target property given these data, incorporating spatial autocorrelation and anisotropy in these models is often not possible. We propose a Gaussian process regression model for 3-D geochemical interpolation, where custom kernels are introduced to integrate collocated 3-D rock property models while addressing the trade-off between the spatial proximity of drill-cores and the similarities in their collocated rock properties, as well as the relative degree to which each supporting 3-D model contributes to interpolation. The proposed model was evaluated for 3-D modelling of Mg content in the Kevitsa Ni-Cu-PGE deposit based on drill-core analyses and four 3-D geophysical inversion models. Incorporating the inversion models improved the regression model's likelihood (relative to a purely spatial Gaussian process regression model) when evaluated at held-out test holes, but only for moderate spatial scales (100 m).http://www.sciencedirect.com/science/article/pii/S1674987120302218Machine learningGaussian process regressionKrigingGeophysical inversionInterpolation
collection DOAJ
language English
format Article
sources DOAJ
author Tom Horrocks
Eun-Jung Holden
Daniel Wedge
Chris Wijns
spellingShingle Tom Horrocks
Eun-Jung Holden
Daniel Wedge
Chris Wijns
3-D geochemical interpolation guided by geophysical inversion models
Geoscience Frontiers
Machine learning
Gaussian process regression
Kriging
Geophysical inversion
Interpolation
author_facet Tom Horrocks
Eun-Jung Holden
Daniel Wedge
Chris Wijns
author_sort Tom Horrocks
title 3-D geochemical interpolation guided by geophysical inversion models
title_short 3-D geochemical interpolation guided by geophysical inversion models
title_full 3-D geochemical interpolation guided by geophysical inversion models
title_fullStr 3-D geochemical interpolation guided by geophysical inversion models
title_full_unstemmed 3-D geochemical interpolation guided by geophysical inversion models
title_sort 3-d geochemical interpolation guided by geophysical inversion models
publisher Elsevier
series Geoscience Frontiers
issn 1674-9871
publishDate 2021-05-01
description 3-D geochemical subsurface models, as constructed by spatial interpolation of drill-core assays, are valuable assets across multiple stages of the mineral industry's workflow. However, the accuracy of such models is limited by the spatial sparsity of the underlying drill-core, which samples only a small fraction of the subsurface. This limitation can be alleviated by integrating collocated 3-D models into the interpolation process, such as the 3-D rock property models produced by modern geophysical inversion procedures, provided that they are sufficiently resolved and correlated with the interpolation target. While standard machine learning algorithms are capable of predicting the target property given these data, incorporating spatial autocorrelation and anisotropy in these models is often not possible. We propose a Gaussian process regression model for 3-D geochemical interpolation, where custom kernels are introduced to integrate collocated 3-D rock property models while addressing the trade-off between the spatial proximity of drill-cores and the similarities in their collocated rock properties, as well as the relative degree to which each supporting 3-D model contributes to interpolation. The proposed model was evaluated for 3-D modelling of Mg content in the Kevitsa Ni-Cu-PGE deposit based on drill-core analyses and four 3-D geophysical inversion models. Incorporating the inversion models improved the regression model's likelihood (relative to a purely spatial Gaussian process regression model) when evaluated at held-out test holes, but only for moderate spatial scales (100 m).
topic Machine learning
Gaussian process regression
Kriging
Geophysical inversion
Interpolation
url http://www.sciencedirect.com/science/article/pii/S1674987120302218
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AT eunjungholden 3dgeochemicalinterpolationguidedbygeophysicalinversionmodels
AT danielwedge 3dgeochemicalinterpolationguidedbygeophysicalinversionmodels
AT chriswijns 3dgeochemicalinterpolationguidedbygeophysicalinversionmodels
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