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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Autores principales:	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
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/60fafb0c2e2f4cd28c7f73596751a4d7
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spelling	oai:doaj.org-article:60fafb0c2e2f4cd28c7f73596751a4d72021-12-02T18:03:13ZOxidized sulfur-rich arc magmas formed porphyry Cu deposits by 1.88 Ga10.1038/s41467-021-22349-z2041-1723https://doaj.org/article/60fafb0c2e2f4cd28c7f73596751a4d72021-04-01T00:00:00Zhttps://doi.org/10.1038/s41467-021-22349-zhttps://doaj.org/toc/2041-1723Tectonomagmatic 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.Xuyang MengJackie M. KleinsasserJeremy P. RichardsSimon R. TapsterPedro J. JugoAdam C. SimonDaniel J. KontakLaurence RobbGrant M. BybeeJeffrey H. MarshRichard A. SternNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-9 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q 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
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.
format	article
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
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 Portfolio
publishDate	2021
url	https://doaj.org/article/60fafb0c2e2f4cd28c7f73596751a4d7
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Oxidized sulfur-rich arc magmas formed porphyry Cu deposits by 1.88 Ga

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