[J06-P] Poster

[J06-P-03] Shallow Slow Slip Event Off the Kii Peninsula, Japan

^○Satoshi Itaba¹, Satoshi Annoura², Tetsuo Hashimoto², Noriko Kamaya², Akio Katsumata³ (1.National Institute of Advanced Industrial Science and Technology, Tsukuba, Japan, 2.Japan Meteorological Agency, Tokyo, Japan, 3.Meteorological Research Institute, Tsukuba, Japan)

On 1 April 2016, an earthquake (Mw=5.9, hereafter mainshock, USGS) occurred off the Kii Peninsula, Japan. The mainshock occurred around the expected focal region of the so-called Tonankai earthquake. After the mainshock, strain changes caused by the slow slip event (SSE) were observed by the three borehole strainmeters of AIST. The source region of this SSE is located on the plate interface at southeast side of the mainshock. An equivalent magnitude of this SSE is Mw 6.0, and duration is about 7 days. From after just a few days from the mainshock, in and around this SSE source region, intensive activity of shallow low frequency tremor (LFT) has been observed for about two weeks, it is assumed that these shallow tremor events were induced by this SSE.
In off the Kii Peninsula, SSE had not been observed by geodetic method. The slip deficit rate of this SSE source region is about 3 cm / year (Yokota et al., 2016), and the plate convergence rate is 5.0 to 6.5 cm / year (Heki and Miyazaki, 2001). Therefore, in addition to this case, there is a possibility that SSE frequently occurred in this region. To support of this hypothesis, VLF and LFT have been often observed in this area. In this presentation, we will report the results of verifying other cases.

References
Heki, K. and S. Miyazaki, Plate Convergence and Long-Term Crustal Deformation in Central Japan,. Geophys. Res. Lett., 28, 2313-2316, 2001.
Yokota, Y., T. Ishikawa, S. Watanabe, T. Tashiro, and A. Asada, Seafloor geodetic constraints on interplate coupling of the Nankai Trough megathrust zone, Nature, 534, 374-377, doi:10.1038/nature17632, 2016.