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

Funding

National Natural Science Foundation of China

42376051

National Natural Science Foundation of China

42006049

National Natural Science Foundation of China

91958215

Natural Science Foundation of Shandong Province

ZR2020MD029

Shandong Basic Research Office

WSR2023018

Higher Education Discipline Innovation Project

B18048

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