Research data for: Sedimentary history and provenance analysis of the Sanbagawa Belt in eastern Kii Peninsula, Southwest Japan, based on detrital zircon U–Pb ages

Published: 13 March 2020| Version 1 | DOI: 10.17632/3xjdbvwgcf.1
Contributor:
Sui JIA

Description

Supplementary material: U–Pb isotope data for zircons analyzed in this study. Uncertainties are given at the 2σ level. %conc = 100 × (238U–206Pb age)/(235U–207Pb age) is the measure of concordance between 238U–206Pb and 235U–207Pb ages. Shading indicates discordant data, which were not included in the probability density plots or histograms.

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Accretionary Wedge, Zircon, Chronology

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