浅発地震の走時による日本の表層構造 (續)

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書誌事項

タイトル別名
  • The Crustal Structure Derived from the Travel Time of Shallow Earthquakes. (continued)
  • 地震波による地殻構造の研究-2-
  • ジシンハ ニ ヨル チカク コウゾウ ノ ケンキュウ 2
  • （地震波による地殼構造の研究 2）

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抄録

This is continued from the previous paper of the same title. Summary of the present paper is as follows. (1) Corrections and additions to the Crustal structure . which mentioned in the previous paper are shown in Figure 1. (2) Horizotal structures at the surface and at the depth of 10km., 20km., 30km., and 40km. are derived from the vertical structures, and illustrated in Figure 3-7. (3) The distributions of observed gravity anomalies are well consistent with the lateral structure of the crust now determined by the author's. (4) The analogies between geological structures and the author's one are discussed. The median line and Fossa Magna are able to point out in the vertical structures. (5) The observed deviations of incident times of P waves of deep earthquakes agree well with the same deviations calculated from the author's structures. The last problem will be mentioned again in the following paper.

収録刊行物

  • 地震　第２輯

    地震　第２輯 7 (4), 226-232, 1955

    公益社団法人 日本地震学会

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