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Apatite fission-track and (U-Th)/He ages of the Suzuka Range, southwest Japan, and their geomorphological implications

Sueoka, Shigeru   ; Yamada, Kunimi; Shibata, Kenji; Tsutsumi, Hiroyuki*; Tagami, Takahiro*; Hasebe, Noriko*; Tamura, Akihiro*; Arai, Shoji*

We are attempting to reveal uplift and denudation history of the Suzuka Range, southwest Japan, by using apatite fission-track and (U-Th)/He thermochronology. The Suzuka Range is distributed along the tectonic boundary of the reverse fault dominant Kinki district and strike-slip fault dominant Chubu district, which is thought to be a reflection of the Philippine Sea Plate slab geometry in this area. We are planning to reconstruct uplift and denudation history of the Suzuka Range in the past few million years and discuss its geomorphological and tectonic implications.

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