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
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.
Accretionary Wedge, Zircon, Chronology