大垣市周辺の常時微動特性と地質図について

概要

論文の詳細を見る
In this measurement, all measurement points are set at the the very point of the tower for power grid. Therefore, measurment lines are automatically decided. Moreover, these points are easily determined on the geological maps drawn when those towers were constructed. The microtremors covering a wide area at the northwest part of the Nobi plain were measured and analyzed and those superior frequencies were compared with that geological map. In the case of homogenous soil layer, superior frequencies show the same value everywhere on it. In the case of unhomogenous, superior frequencies show several values which are charactristic of the soil. It seems that a correlation exists between those superior frequencies and the geolgical map at several points.
岐阜工業高等専門学校の論文
1985-03-20