Oxidized sulfur-rich arc magmas formed porphyry Cu deposits by 1.88 Ga

Tectonomagmatic conditions in the Precambrian were hypothesized to be unfavorable for porphyry Cu deposit formation. Here, the authors show that metallogenic processes typify Phanerozoic porphyry Cu deposits operated by ~1.88 Ga, reflecting modification of mantle lithosphere by oxidized slab-derived...

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Main Authors:	Xuyang Meng, Jackie M. Kleinsasser, Jeremy P. Richards, Simon R. Tapster, Pedro J. Jugo, Adam C. Simon, Daniel J. Kontak, Laurence Robb, Grant M. Bybee, Jeffrey H. Marsh, Richard A. Stern
Format:	Article
Language:	English
Published:	Nature Publishing Group 2021-04-01
Series:	Nature Communications
Online Access:	https://doi.org/10.1038/s41467-021-22349-z

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spelling	doaj-60fafb0c2e2f4cd28c7f73596751a4d72021-04-18T11:13:02ZengNature Publishing GroupNature Communications2041-17232021-04-011211910.1038/s41467-021-22349-zOxidized sulfur-rich arc magmas formed porphyry Cu deposits by 1.88 GaXuyang Meng0Jackie M. Kleinsasser1Jeremy P. Richards2Simon R. Tapster3Pedro J. Jugo4Adam C. Simon5Daniel J. Kontak6Laurence Robb7Grant M. Bybee8Jeffrey H. Marsh9Richard A. Stern10Mineral Exploration Research Centre, Harquail School of Earth Sciences, Laurentian UniversityDepartment of Earth and Environmental Sciences, University of MichiganMineral Exploration Research Centre, Harquail School of Earth Sciences, Laurentian UniversityGeochronology and Tracers Facility, British Geological SurveyMineral Exploration Research Centre, Harquail School of Earth Sciences, Laurentian UniversityDepartment of Earth and Environmental Sciences, University of MichiganMineral Exploration Research Centre, Harquail School of Earth Sciences, Laurentian UniversityDepartment of Earth Sciences, University of OxfordSchool of Geosciences, University of WitwatersrandMineral Exploration Research Centre, Harquail School of Earth Sciences, Laurentian UniversityCanadian Centre for Isotopic Microanalysis, University of AlbertaTectonomagmatic conditions in the Precambrian were hypothesized to be unfavorable for porphyry Cu deposit formation. Here, the authors show that metallogenic processes typify Phanerozoic porphyry Cu deposits operated by ~1.88 Ga, reflecting modification of mantle lithosphere by oxidized slab-derived fluids at that time.https://doi.org/10.1038/s41467-021-22349-z
collection	DOAJ
language	English
format	Article
sources	DOAJ
author	Xuyang Meng Jackie M. Kleinsasser Jeremy P. Richards Simon R. Tapster Pedro J. Jugo Adam C. Simon Daniel J. Kontak Laurence Robb Grant M. Bybee Jeffrey H. Marsh Richard A. Stern
spellingShingle	Xuyang Meng Jackie M. Kleinsasser Jeremy P. Richards Simon R. Tapster Pedro J. Jugo Adam C. Simon Daniel J. Kontak Laurence Robb Grant M. Bybee Jeffrey H. Marsh Richard A. Stern Oxidized sulfur-rich arc magmas formed porphyry Cu deposits by 1.88 Ga Nature Communications
author_facet	Xuyang Meng Jackie M. Kleinsasser Jeremy P. Richards Simon R. Tapster Pedro J. Jugo Adam C. Simon Daniel J. Kontak Laurence Robb Grant M. Bybee Jeffrey H. Marsh Richard A. Stern
author_sort	Xuyang Meng
title	Oxidized sulfur-rich arc magmas formed porphyry Cu deposits by 1.88 Ga
title_short	Oxidized sulfur-rich arc magmas formed porphyry Cu deposits by 1.88 Ga
title_full	Oxidized sulfur-rich arc magmas formed porphyry Cu deposits by 1.88 Ga
title_fullStr	Oxidized sulfur-rich arc magmas formed porphyry Cu deposits by 1.88 Ga
title_full_unstemmed	Oxidized sulfur-rich arc magmas formed porphyry Cu deposits by 1.88 Ga
title_sort	oxidized sulfur-rich arc magmas formed porphyry cu deposits by 1.88 ga
publisher	Nature Publishing Group
series	Nature Communications
issn	2041-1723
publishDate	2021-04-01
description	Tectonomagmatic conditions in the Precambrian were hypothesized to be unfavorable for porphyry Cu deposit formation. Here, the authors show that metallogenic processes typify Phanerozoic porphyry Cu deposits operated by ~1.88 Ga, reflecting modification of mantle lithosphere by oxidized slab-derived fluids at that time.
url	https://doi.org/10.1038/s41467-021-22349-z
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Oxidized sulfur-rich arc magmas formed porphyry Cu deposits by 1.88 Ga

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