10Be dating of middle-late Pleistocene uplifted marine terraces in northern Pacific coast of Northeastern Japan
- 1Hirosaki University, Institute of Regional Innovation, Hirosaki, Japan (wakasa@hirosaki-u.ac.jp)
- 2Earthquake Research Institute, University of Tokyo, Bunkyo-ku, Tokyo, Japan (ishiyama@eri.u-tokyo.ac.jp)
- 3Faculty of Education, Shinshu University, Nagano, Japan (hirokuma@shinshu-u.ac.jp)
- 4Faculty of Education, Okayama University, Okayama, Japan (pj4c33ry@s.okayama-u.ac.jp)
- 5Tono Geoscience center, Japan Atomic Energy Agency, Toki, Gifu, Japan (fujita.natsuko@jaea.go.jp)
- 6Kankyo Chisitsu, Co., Ltd, Kawasaki, Kanagawa, Japan (echigo@kankyo-c.com)
Surface exposure ages of marine and fluvial terraces based on in situ 10Be dating were determined to estimate formation ages and long-term rates of coastal uplift along the northern Pacific coast of Northeastern Japan. Surface rock samples were collected along the northern and southern coasts of Sanriku based on a reinterpretation of dispersed marine and fluvial terraces using DEM and aerial photographs. We collected three samples at the Samuraihama site from outcrops of pairs of marine and fluvial terraces distributed over the east-facing flank of the Kitakami Mountains. At the Yoshihama site, in contrast, where bedrock surfaces could be better exposed, we took vertical samples from weathered granite rocks on small trench walls dug on the middle marine terrace at Yoshihama Bay. Surface exposure ages from 10Be concentrations in quartz calculated from the measured 10Be/9Be ratios commonly suggest slow in both sites, whereas steep (~ 10°) dip domains on the marine terraces along the northern Sanriku coast may imply localized permanent strain accumulation.
How to cite: Wakasa, S., Ishiyama, T., Hirouchi, D., Matta, N., Fujita, N., and Echigo, T.: 10Be dating of middle-late Pleistocene uplifted marine terraces in northern Pacific coast of Northeastern Japan, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-10655, https://doi.org/10.5194/egusphere-egu23-10655, 2023.