The gold content of mafic to felsic potassic magmas

Abstract Many epithermal gold and gold-rich porphyry-type ore deposits are associated with potassic magmas. Hence, potassic magmas are commonly assumed to have been unusually Au-rich or to have contained high Au/Cu ratios. However, these hypotheses remain poorly tested. Here, we report Au concentrat...

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Main Authors: Jia Chang, Andreas Audétat, Thomas Pettke
Format: Article
Language:English
Published: Nature Portfolio 2024-08-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-024-51405-7
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author Jia Chang
Andreas Audétat
Thomas Pettke
author_facet Jia Chang
Andreas Audétat
Thomas Pettke
author_sort Jia Chang
collection DOAJ
description Abstract Many epithermal gold and gold-rich porphyry-type ore deposits are associated with potassic magmas. Hence, potassic magmas are commonly assumed to have been unusually Au-rich or to have contained high Au/Cu ratios. However, these hypotheses remain poorly tested. Here, we report Au concentrations and Au/Cu ratios in silicate melt inclusions analyzed in potassic rocks worldwide. The results suggest that mafic potassic magmas generally contain only 2‒7 ng/g Au, despite common sulfide exhaustion during partial mantle melting. Both the absolute Au concentrations and Au/Cu ratios are comparable to those of mafic calc-alkaline magmas, and they vary little during subsequent magma differentiation because magmatic sulfide precipitation is strongly dominated by monosulfide solid solution that is relatively poor in Au and Cu. We thus suggest that the close association of Au-rich deposits with potassic magmas is not due to Au enrichment in the magma, but rather due to selective Au precipitation at the hydrothermal stage.
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spelling doaj-art-1fb18753007f49e0ba7e15e6493ff2cb2025-02-02T12:31:00ZengNature PortfolioNature Communications2041-17232024-08-0115111010.1038/s41467-024-51405-7The gold content of mafic to felsic potassic magmasJia Chang0Andreas Audétat1Thomas Pettke2Bavarian Geoinstitute, University of BayreuthBavarian Geoinstitute, University of BayreuthInstitute of Geological Sciences, University of BernAbstract Many epithermal gold and gold-rich porphyry-type ore deposits are associated with potassic magmas. Hence, potassic magmas are commonly assumed to have been unusually Au-rich or to have contained high Au/Cu ratios. However, these hypotheses remain poorly tested. Here, we report Au concentrations and Au/Cu ratios in silicate melt inclusions analyzed in potassic rocks worldwide. The results suggest that mafic potassic magmas generally contain only 2‒7 ng/g Au, despite common sulfide exhaustion during partial mantle melting. Both the absolute Au concentrations and Au/Cu ratios are comparable to those of mafic calc-alkaline magmas, and they vary little during subsequent magma differentiation because magmatic sulfide precipitation is strongly dominated by monosulfide solid solution that is relatively poor in Au and Cu. We thus suggest that the close association of Au-rich deposits with potassic magmas is not due to Au enrichment in the magma, but rather due to selective Au precipitation at the hydrothermal stage.https://doi.org/10.1038/s41467-024-51405-7
spellingShingle Jia Chang
Andreas Audétat
Thomas Pettke
The gold content of mafic to felsic potassic magmas
Nature Communications
title The gold content of mafic to felsic potassic magmas
title_full The gold content of mafic to felsic potassic magmas
title_fullStr The gold content of mafic to felsic potassic magmas
title_full_unstemmed The gold content of mafic to felsic potassic magmas
title_short The gold content of mafic to felsic potassic magmas
title_sort gold content of mafic to felsic potassic magmas
url https://doi.org/10.1038/s41467-024-51405-7
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