Machine-learning crystal size distribution for volcanic stratigraphy correlation

Abstract Volcanic stratigraphy reconstruction is traditionally based on qualitative facies analysis complemented by geochemical analyses. Here we present a novel technique based on machine learning identification of crystal size distribution to quantitatively fingerprint lavas, shallow intrusions an...

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Main Authors: Martin Jutzeler, Rebecca J. Carey, Yasin Dagasan, Andrew McNeill, Ray A. F. Cas
Format: Article
Language:English
Published: Nature Portfolio 2024-12-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-024-82847-0
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author Martin Jutzeler
Rebecca J. Carey
Yasin Dagasan
Andrew McNeill
Ray A. F. Cas
author_facet Martin Jutzeler
Rebecca J. Carey
Yasin Dagasan
Andrew McNeill
Ray A. F. Cas
author_sort Martin Jutzeler
collection DOAJ
description Abstract Volcanic stratigraphy reconstruction is traditionally based on qualitative facies analysis complemented by geochemical analyses. Here we present a novel technique based on machine learning identification of crystal size distribution to quantitatively fingerprint lavas, shallow intrusions and coarse lava breccias. This technique, based on a simple photograph of a rock (or core) sample, is complementary to existing methods and allows another strategy to identify and compare volcanic rocks for stratigraphic correlation. Phenocryst size distributions display overall homogeneity within one volcanic body but may vary considerably between igneous bodies. Restricted to shallow intrusions and volcanic lavas, this concept allows for stratigraphic fingerprinting of volcanic rocks in poorly exposed, up to moderately altered, and/or complexly tectonized formations. We built an automated image analysis workflow using machine-learning for crystal segmentation, followed by statistical analysis of physical descriptors to compare and match the size distribution of feldspar phenocrysts. The workflow comprises three instance segmentation models for pre-processing the images, automated scale measurement and grain segmentation using Mask R-CNN. This avoids the laborious and time-consuming task of manual picking by image analysis, and allows for a rapid, unbiased and quantitative approach to determine crystal size distribution (CSD). Our volcanic architecture reconstruction of multiple dacite bodies in the mineralized Cambrian Mt Read Volcanics in Tasmania, Australia, is independently validated by bulk-rock chemical analyses of key samples. This volcanic stratigraphy method can be applied to a large variety of igneous rocks and is complementary to geochemical analyses and qualitative crystal content assessment.
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spelling doaj-art-5254e0af6477442b88e46c289265b9ac2025-01-05T12:29:49ZengNature PortfolioScientific Reports2045-23222024-12-0114111010.1038/s41598-024-82847-0Machine-learning crystal size distribution for volcanic stratigraphy correlationMartin Jutzeler0Rebecca J. Carey1Yasin Dagasan2Andrew McNeill3Ray A. F. Cas4Centre for Ore Deposit and Earth Sciences, School of Natural Sciences, University of TasmaniaCentre for Ore Deposit and Earth Sciences, School of Natural Sciences, University of TasmaniaDatarock Pty LtdGeological Survey Branch, Mineral Resources TasmaniaCentre for Ore Deposit and Earth Sciences, School of Natural Sciences, University of TasmaniaAbstract Volcanic stratigraphy reconstruction is traditionally based on qualitative facies analysis complemented by geochemical analyses. Here we present a novel technique based on machine learning identification of crystal size distribution to quantitatively fingerprint lavas, shallow intrusions and coarse lava breccias. This technique, based on a simple photograph of a rock (or core) sample, is complementary to existing methods and allows another strategy to identify and compare volcanic rocks for stratigraphic correlation. Phenocryst size distributions display overall homogeneity within one volcanic body but may vary considerably between igneous bodies. Restricted to shallow intrusions and volcanic lavas, this concept allows for stratigraphic fingerprinting of volcanic rocks in poorly exposed, up to moderately altered, and/or complexly tectonized formations. We built an automated image analysis workflow using machine-learning for crystal segmentation, followed by statistical analysis of physical descriptors to compare and match the size distribution of feldspar phenocrysts. The workflow comprises three instance segmentation models for pre-processing the images, automated scale measurement and grain segmentation using Mask R-CNN. This avoids the laborious and time-consuming task of manual picking by image analysis, and allows for a rapid, unbiased and quantitative approach to determine crystal size distribution (CSD). Our volcanic architecture reconstruction of multiple dacite bodies in the mineralized Cambrian Mt Read Volcanics in Tasmania, Australia, is independently validated by bulk-rock chemical analyses of key samples. This volcanic stratigraphy method can be applied to a large variety of igneous rocks and is complementary to geochemical analyses and qualitative crystal content assessment.https://doi.org/10.1038/s41598-024-82847-0
spellingShingle Martin Jutzeler
Rebecca J. Carey
Yasin Dagasan
Andrew McNeill
Ray A. F. Cas
Machine-learning crystal size distribution for volcanic stratigraphy correlation
Scientific Reports
title Machine-learning crystal size distribution for volcanic stratigraphy correlation
title_full Machine-learning crystal size distribution for volcanic stratigraphy correlation
title_fullStr Machine-learning crystal size distribution for volcanic stratigraphy correlation
title_full_unstemmed Machine-learning crystal size distribution for volcanic stratigraphy correlation
title_short Machine-learning crystal size distribution for volcanic stratigraphy correlation
title_sort machine learning crystal size distribution for volcanic stratigraphy correlation
url https://doi.org/10.1038/s41598-024-82847-0
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