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Iron isotope fractionation during mid-ocean ridge basalt (MORB) evolution: Evidence from lavas on the East Pacific Rise at 10°30′N and its implications

Crossref DOI link: https://doi.org/10.1016/j.gca.2019.09.031

Published Print: 2019-12

Update policy: https://doi.org/10.1016/elsevier_cm_policy

Authors

Chen, Shuo https://orcid.org/0000-0002-8365-2500
Niu, Yaoling https://orcid.org/0000-0001-9488-2304
Guo, Pengyuan

Gong, Hongmei

Sun, Pu

Xue, Qiqi

Duan, Meng

Wang, Xiaohong
Funding

Funding for this research was provided by:

China Postdoctoral Science Foundation

National Natural Science Foundation of China

National Natural Science Foundation of China-Shandong Joint Fund for Marine Science Research Centers

Higher Education Discipline Innovation Project
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Text and Data Mining valid from 2019-12-01

Text and Data Mining valid from 2019-12-01
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This article is maintained by: Elsevier

Article Title: Iron isotope fractionation during mid-ocean ridge basalt (MORB) evolution: Evidence from lavas on the East Pacific Rise at 10°30′N and its implications

Journal Title: Geochimica et Cosmochimica Acta

CrossRef DOI link to publisher maintained version: https://doi.org/10.1016/j.gca.2019.09.031

Content Type: article

Copyright: © 2019 Elsevier Ltd. All rights reserved.

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