Fluid metasomatic rocks with extremely low δ26Mg values in the subducted oceanic lithosphere: Implications for mantle Mg isotope heterogeneity and the origin of low-δ26Mg magmas

Name: Fluid metasomatic rocks with extremely low δ26Mg values in the subducted oceanic lithosphere: Implications for mantle Mg isotope heterogeneity and the origin of low-δ26Mg magmas
Creator: Jia-Wei Xiong
Published: 2023-11-21T08:52:28.313Z
Keywords: Geochemistry, Serpentine, Stable Isotope, Subduction Zone

Xiong, Jia-Wei; Chen, Yi-Xiang; Scambelluri, Marco; Qiao, Xin-Yue; Chen, Yu; Huang, Fang; Zhao, Zi-Fu

doi:10.17632/h5sbhtc3np.2

Fluid metasomatic rocks with extremely low δ26Mg values in the subducted oceanic lithosphere: Implications for mantle Mg isotope heterogeneity and the origin of low-δ26Mg magmas

Published: 21 November 2023| Version 2 | DOI: 10.17632/h5sbhtc3np.2

Contributors:

Jia-Wei Xiong, Yi-Xiang Chen, Marco Scambelluri, Xin-Yue Qiao, Yu Chen, Fang Huang, Zi-Fu Zhao

Description

The files contain: Table1 for Whole-rock Mg-O-Sr-Nd isotope compositions of the studied Ti-clinohumite dikelets, metarodingites and related serpentinites and Table S1 for Whole-rock trace element compositions of the studied samples.

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University of Science and Technology of China

Fluid metasomatic rocks with extremely low δ26Mg values in the subducted oceanic lithosphere: Implications for mantle Mg isotope heterogeneity and the origin of low-δ26Mg magmas

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