Shallow subsurface structure estimated from dense aftershock records and microtremor observations in Furukawa district, Miyagi, Japan
| Autor: | Koji Hada, Hiroyuki Goto, Hitoshi Mitsunaga, Masayuki Inatani, Toshiyasu Takaya, Takaaki Ikeda, Sayaka Kimura, Kahori Iiyama, Hitoshi Morikawa, Sumio Sawada, Ryohei Akiyama |
|---|---|
| Rok vydání: | 2017 |
| Předmět: |
Seismometer
010504 meteorology & atmospheric sciences Geology 010502 geochemistry & geophysics Spatial distribution 01 natural sciences Basement symbols.namesake Geophysics symbols Microtremor Rayleigh wave Phase velocity Aftershock Seismology 0105 earth and related environmental sciences Refraction microtremor |
| Zdroj: | Exploration Geophysics. 48:16-27 |
| ISSN: | 1834-7533 0812-3985 |
| DOI: | 10.1071/eg16113 |
| Popis: | We conducted single-site and array observations of microtremors in order to revise the shallow subsurface structure of the Furukawa district, Miyagi, Japan, where severe residential damage was reported during the Great Eastern Japan Earthquake of 2011, off the Pacific coast of Tohoku. The phase velocities of Rayleigh waves are estimated from array observations at three sites, and S-wave velocity models are established. The spatial distribution of predominant periods is estimated for the surface layer, on the basis of the spectral ratio of horizontal and vertical components (H/V) of microtremors obtained from single-site observations. We then compared ground motion records from a dense seismometer network with results of microtremor observations, and revised a model of the shallow (~100 m) subsurface structure in the Furukawa district. The model implies that slower near-surface S-wave velocity and deeper basement are to be found in the southern and eastern areas. It was found that the damage in residential structures was concentrated in an area where the average value for the transfer functions in the frequency range of 2 to 4 Hz was large. |
| Databáze: | OpenAIRE |
| Externí odkaz: |
|