Most of the current seismological studies of the fne structure of the Earth's deep interior has been made from direct measurements of apparent velocity with the mounting use of seismological arrays of considerable linear dimensions with identical seismographs. In spjte of a considerable dimension of the network and identical seismographs of Dodaira Micro-Earthquake Observatory, the stations of the network are distributed too sparse to make the direct measurement of apparent velocity.
雑誌名
地震研究所研究速報
巻
12
ページ
57 - 71
発行年
1974-03
書誌レコードID
AN10165194
日本十進分類法
051.1
出版者
東京大学地震研究所
出版者別名
Earthquake Research Institute, University of Tokyo
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