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Cooling history of a fracture zone distributed in the Kojyaku granite, Tsuruga area; Constraints from multi-system thermochronometry

Sueoka, Shigeru   ; Yasue, Kenichi; Niwa, Masakazu   ; Shimada, Koji   ; Ishimaru, Tsuneari ; Umeda, Koji; Yamada, Ryuji*; Danhara, Toru*; Iwano, Hideki*; Gozu, Chitaro*

We introduce an attempt to date a fault distributed in the Kojyaku granite, Tsuruga area, by reconstructing its cooling history based on multi-system thermochronology. The U-Pb ages, zircon fission-track ages, and zircon fission-track length distributions of the fault gauge and host granitic rock indicate a common cooling history at higher temperature, whereas apatite fission-track may imply later reheating in the fault gauge. We are planning to provide more definitive discussions based on apatite fission-track length data.

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