Information on the whole rock chemical composition and U-Pb zircon ages of the Takata granodiorite and related rocks in Southwest Japan

<div><strong>1.</strong> Locations of samples analyzed by XRF and for which U–Pb zircon ages have been obtained.</div> <p><br></p> <div><strong>2. </strong>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.</div> <p><br></p> <div><strong>3.</strong> 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.  </div> <p><br></p> <div><strong>4.</strong> (a) U–Pb isotope Tera–Wasserburg concordia diagrams, (b) probability density of U–Pb ages, and (c) age distribution plots for sample OD-3.</div>