Abstract
MIHARA-YAMA is a basaltic stratovolcano on Oshima, an island lying about 20 km off the coast of Izu Peninsula in central Japan (Fig. 1). I attempt here to show that the magmatic activity of Mihara-yama could be used to predict large earthquakes along the Sagami Trough. There is apparently a causal relationship between eruptions of Mihara-yama and the earthquakes.
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Nakamura, K., Bull. volcan. Soc. Japan, 16, 63–71 (1971).
Sugimura, A., Kagaku, 42, 192–202 (1972).
Kanamori, H., and Ando, M., Publs 50th Anniversary of the Great Kanto Earthquake, 1923, 89–101 (Earthquake Research Institute, University of Tokyo, 1973).
Kimura, M., J. Geogr., 82, 171–188 (1973).
Kimura, M., and Toyoda, J., Bull. volcan. Soc. Japan, 19, 65–78 (1975).
Nagumo, S., Publs 50th Anniversary of the Great Kanto Earthquake, 1923, 273–291 (Earthquake Research Institute, University of Tokyo, 1973).
Tsuya, H., Okada, A., and Watanabe, T., Bull Earthq. Res. Inst., Tokyo Univ., 34, 33–59 (1956).
Kizawa, T., and Tanaka, Y., Pap. Meteorol. Geophys., 23, 411–428 (1972).
Fujita, N., Rep. coord. Comm. Earthquake Prediction, 5, 36–37 (1971).
Imamura, A., Publs Imp. Earthq. invest. Comm., 25, 1–143 (1930).
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KIMURA, M. Major magmatic activity as a key to predicting large earthquakes along the Sagami Trough, Japan. Nature 260, 131–133 (1976). https://doi.org/10.1038/260131b0
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DOI: https://doi.org/10.1038/260131b0
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