Japan Geoscience Union Meeting 2014

Presentation information

Oral

Symbol S (Solid Earth Sciences) » S-SS Seismology

[S-SS35_2PM1] Recent developments in microtremor surveys

Fri. May 2, 2014 2:15 PM - 4:00 PM 502 (5F)

Convener:*Hisashi Nakahara(Solid Earth Physics Laboratory, Department of Geophysics, Graduate School of Science, Tohoku University), Hiroaki Sato(Central Research Institute of Electric Power Industry), Chair:Hisashi Nakahara(Solid Earth Physics Laboratory, Department of Geophysics, Graduate School of Science, Tohoku University), Hiroaki Sato(Central Research Institute of Electric Power Industry)

3:05 PM - 3:20 PM

[SSS35-P05_PG] Estimation of Subsurface Structure using Microtremor Observation in Ogasawara Iwo-To Island

3-min talk in an oral session

*Takumi MURAKOSHI1, Etsuro KOMORI1, Masaki SHIMADA1 (1.National Defense Academy)

Keywords:microtremor, Ogasawara Iwo-To Island, subsurface structure

Ogasawara Iwo-To island is an active volcanic island which is located on the southernmost part of Izu-Ogasawara arc. The microtermor obserbation was carried out during the period from December 18 to 21, 2013 in Ogasawara Iwo-To island. The microtremor measurements were performed at 54 sites as 3-component seismometers for horizontal-to-vertical spectral ratio (HVSR) analysis. The obtained HVSRs of microtremor are used to determine the dominant frequencies of vibration of the subsurface structures beneath several recording sites in Ogasawara Iwo-To island. The H/V peak period varies from 1.1 to 3.5 sec.For using the SPAC method of microtremor, the circular-array microtremor data were recorded by 6 seismometers distributed along the circumferences of two circles as well as a seismometer deployed in the center at two sites in the center of the island. The phase velocities and the S-wave velocities of the subsurface structures down to a depth of several km were estimated at each site from the microtremor data by using the SPAC method.