- 著者
-
一柳 昌義
シェスタコフ ニコライ
奥山 哲
大園 真子
笠原 稔
高橋 浩晃
- 出版者
- 北海道大学大学院理学研究院
- 雑誌
- 北海道大学地球物理学研究報告 (ISSN:04393503)
- 巻号頁・発行日
- vol.81, pp.17-26, 2018-03-19
A M5.6 shallow earthquake occurred on 8 July 2014 in middle east Iburi region, southwestern Hokkaido. Maximum seismic intensity of 5- was observed at Shiraoi town. Three temporal seismic stations had been installed in the focal region from 9 July 2014 to 30 April 2015. We determined 384 aftershock hypocenters by the double-difference tomographic hypocenter determination with proper seismic velocity structure. Relocated aftershocks were clearly distributed on a southeastern ward dipping plane with 5~10 km depth. This configuration agreed with a nodal plane of mainshock focal mechanism. Aftershocks occurred in surrounding part of a low seismicity patch. Mainshock was located deepest part of aftershock zone. These facts suggested that mainshock rupture propagated from deep to shallow, and a low seismicity patch was mainshock slip area. No clear correlation between this earthquake sequence and nearest active Tarumae volcano activity were identified.