TY - JOUR A1 - Ogasawara, Masatsugu A1 - Fukuyama, Mayuko A1 - Horie, Kenji A1 - Sumii, Tomoaki A1 - Takehara, Mami A1 - Sudo, Masafumi T1 - SHRIMP U-Pb age of SoriZ93 zircon from the Sori Granodiorite, Northeast Japan: a potential reference zircon of Late Cretaceous age T2 - ISLAND ARC N2 - SoriZ93 zircon was separated from residual mineral fraction after the preparation of the SORI93 biotite standard from the Sori Granodiorite in the Ashio Mountains, Northeast Japan, and analyzed for its U-Pb age using a sensitive high resolution ion microprobe (SHRIMP). The zircon grains of SoriZ93 are prismatic with pyramidal ends or broken prismatic fragments. Most zircons are 100-250m long and 50-150m wide. The zircons are clear crystals and colorless to pale yellow, although some grains are brown with optically low transparency. Cathodoluminescence (CL) imaging of the SoriZ93 zircons showed a fine oscillatory zoning, which is a typical characteristic of zircons in granitic rocks. A xenocrystic core was not present in the zircons. Although some mineral inclusions were present in the zircons, it is possible to select a typical analytical area with a dimension of 30m necessary for the microbeam technique. The analytical results of the colorless zircons provided a weighted mean Pb-207 corrected Pb-206/U-238 age of 93.9 +/- 0.6Ma (95% confidence, MSWD=0.97). This Pb-206/U-238 age is 1.3m.y. older than the K-Ar age of the SORI93 biotite, indicating that the granodiorite cooled to a closure temperature of the K-Ar biotite system within a short time interval. Although some grains of the SoriZ93 zircons show high U concentration, a selection of colorless zircons provided the precise age to be used for the calibration and reference for zircons of the Late Cretaceous. KW - Late Cretaceous KW - SHRIMP U-Pb dating KW - Sori Granodiorite KW - SoriZ93 KW - zircon standard Y1 - 2013 UR - https://publishup.uni-potsdam.de/frontdoor/index/index/docId/34785 SN - 1038-4871 VL - 22 IS - 3 SP - 306 EP - 317 PB - WILEY-BLACKWELL CY - HOBOKEN ER -