Supplementary tables of Sun et al. submitted to GCA titled "Large correlated zinc isotope variability in the eastern Pacific mantle as a result of low-degree melt metasomatism"

Published: 5 December 2024| Version 1 | DOI: 10.17632/8sjnppnbvj.1
Contributor:
Pu Sun

Description

Description for Supplementary Tables associated with this article: Supplementary Table 1: Major and trace element data of the near-EPR 5-15°N seamount lavas and standard reference materials Supplementary Table 2: Sr-Nd-Pb isotope data of the near-EPR 5-15°N seamount lavas and standard reference materials Supplementary Table 3: Modeling of the Zn isotope variation during partial melting of DMM Supplementary Table 4: Major element abundances corrected for the effect of fractional crystallization to Mg# = ~72 Supplementary Table 5: Estimation for the age of the enriched source component Supplementary Table 5.1: Estimation for the age of the enriched source component with Sr-Nd isotope compositions same as sample CD6-9 with a garnet peridotite lithology Supplementary Table 5.2: Estimation for the age of the enriched source component with more radiogenic Sr-Nd isotope compositions with a garnet peridotite lithology Supplementary Table 5.3: Estimation for the age of the enriched source component with Sr-Nd isotope compositions same as sample CD6-9 with a garnet pyroxenite lithology Supplementary Table 5.4: Estimation for the age of the enriched source component with more radiogenic Sr-Nd isotope compositions with a garnet pyroxenite lithology

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Institutions

Institute of Oceanology Chinese Academy of Sciences

Categories

Igneous Geology, North Pacific, Mid-Ocean Ridge, Seamount, Non-Traditional Isotope Geochemistry

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