The experiment on dating of the tsunami deposits using the luminescence method: A case study of samples from Nemuro coastal lowland, eastern Hokkaido

Author:

Nanayama Futoshi1,Nagatomo Tsuneto2,Shitaoka Yorinao2,Suzaki Ken-ichi2,Furukawa Ryuta1,Shigeno Kiyoyuki3,Ishii Masayuki3,Inokuma Shigeto4,Kitazawa Toshiyuki5,Nakagawa Mitsuru1

Affiliation:

1. Geological Survey of Japan, AIST

2. Department of Science Education, Faculty of Education, Nara University of Education

3. Meiji Consultant Co., Ltd.

4. Nemuro City Museum of History and Nature

5. Department of Geology, Faculty of Science, Shinshu University

Publisher

The Geological Society of Japan

Subject

General Earth and Planetary Sciences,General Engineering,General Environmental Science

Reference36 articles.

1. Adamiec, G. and Aitken, M.J., 1998, Dose-rate conversion factors: update. Ancient TL, 16, 37-50.

2. Aitken, M.J., 1985, Thermoluminesence Dating. Academic Press, London, 351p.

3. Aitken, M.J., 1998, An Introduction to Optical Dating: The Dating of Quaternary Sediments by the Use of Photon-Stimulated Luminescence. Oxford University Press, London, 267p.

4. Ando, A., Mita, N. and Terashima, S., 1987, 1986 values for fifteen GSJ rock reference samples, “igneous rock series”. Geostandards Newsletter, no. 11, 159-166.

5. Banerjee, D., Murray, A. S. and Foster, I. D. L., 2001, Scilly Isles, UK: optical dating of a possible tsunami deposit from the 1755 Lisbon earthquake. Quatern. Sci. Rev., 20, 715-718.

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