Characteristics and generation mechanism of low-frequency earthquakes in the continental plate
Author:
Affiliation:
1. Graduate School of Science and Technology, Hirosaki University
Publisher
The Geological Society of Japan
Link
https://www.jstage.jst.go.jp/article/geosoc/130/1/130_2024.0002/_pdf
Reference177 articles.
1. Abe, Y., Ohkura, T., Shibutani, T., Hirahara, K., Yoshikawa, S. and Inoue, H., 2017, Low-velocity zones in the crust beneath Aso caldera, Kyushu, Japan, derived from receiver function analyses. J. Geophys. Res., B: Solid Earth, 122, 2013–2033.
2. Aizawa, K., Yoshimura, R. and Oshiman, N., 2004, Splitting of the Philippine Sea Plate and a magma chamber beneath Mt. Fuji. Geophys. Res. Lett., 31, L09603, doi: 10.1029/2004GL019477.
3. Aki, K. and Koyanagi, R., 1981, Deep volcanic tremor and magma ascent mechanism under Kilauea, Hawaii. J. Geophys. Res., B: Solid Earth, 86, 7095–7109.
4. Ammon, C. J., 1991, The isolation of receiver effects from teleseismic P waveforms. Bull. Seismol. Soc. Am., 81, 2504–2510.
5. Aoyama, H. and Takeo, M., 2001, Wave properties and focal mechanisms of N-type earthquakes at Asama volcano. J. Volcanol. Geotherm. Res., 105, 163–182.
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