Zircon U-Pb age and Hf-O isotope evidence of the Taihua Complex on the southern margin of the North China Craton: Implications for its magmatic process during the early Paleoproterozoic

Published: 17 September 2024| Version 1 | DOI: 10.17632/zpyp4rmb43.1
Contributor:
Nancy Hui-Chun Chen

Description

Data and Supplementary Information for Chen and others, 2024 - Zircon U-Pb age and Hf-O isotope evidence of the Taihua Complex on the southern margin of the North China Craton: Implications for its magmatic process during the early Paleoproterozoic. Accepted for publication in American Journal of Science. Supplementary Table S1: Summary of the samples and sampling positions in this study. Supplementary Table S2: U-Pb age data for zircons of metamorphic rocks in this study. Supplementary Table S3: Zircon Lu-Hf isotopic compositions of metamorphic rocks in this study. Supplementary Table S4: Zircon O isotopes of metamorphic rocks in this study. Supplementary Table S5: Compilation of zircon U–Pb ages and Hf-O isotopic data of the North China Craton during the ~2.3–2.2 Ga.

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The methods used to obtained the data are found in the published research article.

Institutions

National Cheng Kung University

Categories

Geochronology, Oxygen Isotope

Funding

National Science and Technology Council

NSTC111-2636-M-006-019 and NSTC112-2116-M-006-005-MY2

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