Formation of oxidized sulfur-rich magmas in Neoarchaean subduction zones-Reference-Cited by-同舟云学术

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Formation of oxidized sulfur-rich magmas in Neoarchaean subduction zones

Published:2022-11-28 Issue:12 Volume:15 Page:1064-1070
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nat. Geosci.

Author:

Meng Xuyang^ORCID,Simon Adam C.^ORCID,Kleinsasser Jackie M.,Mole David R.,Kontak Daniel J.,Jugo Pedro J.^ORCID,Mao Jingwen,Richards Jeremy P.

Funder

Canada First Research Excellence Fund

China Scholarship Council

National Science Foundation

U.S. National Science Foundation EAR

National Natural Science Foundation of China

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

https://www.nature.com/articles/s41561-022-01071-5.pdf

Reference80 articles.

1. Edmonds, M. & Wallace, P. J. Volatiles and exsolved vapor in volcanic systems. Elements 13, 29–34 (2017).

2. Wallace, P. J. & Edmonds, M. The sulfur budget in magmas: evidence from melt inclusions, submarine glasses, and volcanic gas emissions. Rev. Mineral. Geochem. 73, 215–246 (2011).

3. Richards, J. P. The oxidation state, and sulfur and Cu contents of arc magmas: implications for metallogeny. Lithos 233, 27–45 (2015).

4. Gaillard, F., Scaillet, B. & Arndt, N. T. Atmospheric oxygenation caused by a change in volcanic degassing pressure. Nature 478, 229–232 (2011).

5. Kelley, K. A. & Cottrell, E. Water and the oxidation state of subduction zone magmas. Science 325, 605–607 (2009).

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