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Oxidation of Archean upper mantle caused by crustal recycling

Lei Gao, Shuwen Liu (), Peter A. Cawood (), Fangyang Hu, Jintuan Wang, Guozheng Sun and Yalu Hu
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Lei Gao: Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University of Geosciences
Shuwen Liu: Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University
Peter A. Cawood: School of Earth, Atmosphere and Environment, Monash University
Fangyang Hu: Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences
Jintuan Wang: State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, CAS
Guozheng Sun: Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University
Yalu Hu: Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University

Nature Communications, 2022, vol. 13, issue 1, 1-7

Abstract: Abstract The redox evolution of Archean upper mantle impacted mantle melting and the nature of chemical equilibrium between mantle, ocean and atmosphere of the early Earth. Yet, the origin of these variations in redox remain controversial. Here we show that a global compilation of ∼3.8-2.5 Ga basalts can be subdivided into group B-1, showing modern mid-ocean ridge basalt-like features ((Nb/La)PM ≥ 0.75), and B-2, which are similar to contemporary island arc-related basalts ((Nb/La)PM

Date: 2022
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DOI: 10.1038/s41467-022-30886-4

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