Sulphide–sulphate stability and melting in subducted sediment and its role in arc mantle redox and chalcophile cycling in space and time-Reference-Cited by-同舟云学术

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Sulphide–sulphate stability and melting in subducted sediment and its role in arc mantle redox and chalcophile cycling in space and time

Published:2017-07 Issue: Volume:470 Page:73-86
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Canil Dante^ORCID,Fellows Steven A.

Funder

Natural Sciences and Engineering Research Council of Canada

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference81 articles.

1. High fO2 during sillimanite zone metamorphism of part of the Barrovian type locality, Glen Clova, Scotland;Ague;J. Petrol.,2002

2. Carbon dioxide released from subduction zones by fluid-mediated reactions;Ague;Nat. Geosci.,2014

3. Sulfur in deep sea sediments (Leg 129) and implications for cycling of sediments in subduction zones;Alt,1992

4. Cycling of sulfur in subduction zones: the geochemistry of sulfur in the Mariana Island Arc and back-arc trough;Alt;Earth Planet. Sci. Lett.,1993

5. The terrestrial uranium isotope cycle;Andersen;Nature,2015

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