Stress-induced spatiotemporal variations in anisotropic structures beneath Hakone volcano, Japan, detected by S wave splitting: A tool for volcanic activity monitoring

• Published in: Journal of geophysical research. Solid earth Vol. 119; no. 9; pp. 7043 - 7057
• Main Authors: Honda, Ryou, Yukutake, Yohei, Yoshida, Akio, Harada, Masatake, Miyaoka, Kazuki, Satomura, Mikio
• Format: Journal Article
• Language: English
• Published: Washington Blackwell Publishing Ltd 01-09-2014
• Subjects: Anisotropy; Calderas; Deformation; Earthquakes; Geophysics; Global positioning systems; GPS; Hot springs; S wave splitting; S waves; Seismic activity; spatiotemporal variations in anisotropy; Splitting; Stations; stress changes; Volcanic activity; Volcanic springs; Volcanoes
• ISSN: 2169-9313; 2169-9356
• DOI: 10.1002/2014JB010978

Hakone volcano, located at the northern tip of the Izu‐Mariana volcanic arc, Japan, has a large caldera structure containing numerous volcanic hot springs. Earthquake swarms have occurred repeatedly within the caldera. The largest seismic swarm since the commencement of modern seismic observations (in 1968) occurred in 2001. We investigated the anisotropic structure of Hakone volcano based on S wave splitting analysis and found spatiotemporal changes in the splitting parameters accompanying the seismic swarm activity. Depth‐dependent anisotropic structures are clearly observed. A highly anisotropic layer with a thickness of ~1.5 km is located beneath the Koziri (KZR) and Kozukayama (KZY) stations. The anisotropic intensity in the region reaches a maximum of 6–7% at a depth of 1 km and decreases markedly to less than 1% at a depth of 2 km. The anisotropic intensity beneath Komagatake station (KOM) decreases gradually from a maximum of 6% at the surface to 0% at a depth of 5 km but is still greater than 2.5% at a depth of 3 km. At KZY, the anisotropic intensity along a travel path of which the back azimuth was the south decreased noticeably after the 2001 seismic swarm activity. During the swarm activity, tilt meters and GPS recorded the crustal deformation. The observed decrease in anisotropic intensity is presumed to be caused by the closing of microcracks by stress changes accompanying crustal deformation near the travel path.
Key Points
Anisotropic structures at a volcano are obtained by S wave splitting analysisTemporal changes of anisotropy relating volcanic activities are detected