Version 2 2024-11-07, 07:18Version 2 2024-11-07, 07:18
Version 1 2024-07-31, 11:08Version 1 2024-07-31, 11:08
dataset
posted on 2024-11-07, 07:18authored bySena Nakayama, Atsushi Kamei, Kenichiro Tani, Chika Iwata, Ai Yakushiji, Koji Matsuba
1. Locations of samples analyzed by XRF and for which U–Pb zircon ages have been obtained.
2. Whole-rock compositions of the Takada granodiorite, the Ogi quartz diorite, and the Shimokuno granite. *Total iron is given as Fe2O3. N.D.: not detected. -: not analyzed. Y: Yakushiji et al. (2012), N: This study.
3. LA–ICP–MS U–Pb data and calculated zircon ages of samples HBGD21, GR10, and OD-3. Pbc and Pb* indicate the common and radiogenic portions, respectively. a Common Pb corrected by assuming 206Pb/238U-208Pb/232Th age-concordance. b Common Pb corrected by assuming 206Pb/238U-207Pb/235U age-concordance.
4. (a) U–Pb isotope Tera–Wasserburg concordia diagrams, (b) probability density of U–Pb ages, and (c) age distribution plots for sample OD-3.