Large iron isotope fractionation during mantle wedge serpentinization: Implications for iron isotopes of arc magmas-Reference-Cited by-同舟云学术

Large iron isotope fractionation during mantle wedge serpentinization: Implications for iron isotopes of arc magmas

Published:2022-04 Issue: Volume:583 Page:117423
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Deng Jianghong^ORCID,He Yongsheng,Zartman Robert E.,Yang Xiaoyong,Sun Weidong

Publisher

Elsevier BV

Subject

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

Reference76 articles.

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4. 4.20 - chemical and isotopic cycling in subduction zones;Bebout,2014

5. Tracking Fe mobility and Fe speciation in subduction zone fluids at the slab-mantle interface in a subduction channel: a tale of whiteschist from the Western Alps;Chen;Geochim. Cosmochim. Acta,2019

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