@article{oai:iwate-u.repo.nii.ac.jp:00009859,
 author = {斎藤, 徳美 and 阿部, 司 and 小林, 直太 and 中島, 直吉 and 中村, 操 and 野越, 三雄 and 毎熊, 輝記},
 issue = {1},
 journal = {物理探査},
 month = {Jan},
 note = {The previous study (Research group for short-and long-period microtremors: 1988), proved that the damage due to soil liquefaction in earthquakes could be estimated by measurements of short-period microtremors. As a series of the previous study, intensive measurements of microtremors and S-wave velocities were made on and around the most heavily damaged areas, Shonan-cho, Hamadori-cho, and Aobacho,in Noshiro City in 1985.
Results of this investigation areas follows:
1) Most of the sites undamaged by soil liquefaction have S-wave velocities above 130m/sec and the ground water level deeper than 3m below the ground surface. 2) Most of the sites damaged by soil liquefaction have S-wave velocities below 130m/sec and the ground water level within 3m below the ground surface. These sites have type a of microtremor spectra, which have peaks above 4Hz, with high probability. 3) It is found that type a of microtremor spectrum corresponds well to the liquefied sites with very shallow level of ground water below the ground surface and very small subsurface S-wave velocities. Therefore, the measurements of short-period microtremors give a high probability prediction of damage from soil liquefaction.},
 pages = {64--75},
 title = {秋田県能代市における地盤の振動特性（2）－1983年日本海中部地震で液状化を生じた地盤の微動特性－},
 volume = {41},
 year = {1988}
}