The horizontally lying slab

Kyoko Okino, Masataka Ando, Satoshi Kaneshima, Kazuro Hirahara

研究成果: Contribution to journalArticle査読

39 被引用数 (Scopus)

抄録

An unusual earthquake (mb=6.2) occurred in the Izu‐Bonin Island region in July 1982. The event, occurring at a depth of 545 km, was clearly separated from the main inclined seismic zone by a distance of about 200 km. To diagnose the situation, we have considered two possibilities: 1) the event might be an unusual event in the sense that its location is unrelated to the position of the subducted slab and that there is probably no slab around it, or 2) the slab, at this depth, might be lying horizontally on top of the 650 km discontinuity, and the unusual event occurred in this horizontal part. Both possibilities have been modeled structurally. We have computed the P‐wave travel times for the present event, as well as for two other events located unambiguously in the inclined part of the seismic zone by employing a 3‐D ray tracing program. The computed travel time residuals have been compared with the observations at stations in western Japan. The observations are found to be consistent with the model of the horizontally lying slab. Our result, thus, suggests that the slab might be horizontal at this depth in this part of the Izu‐Bonin Islands.

本文言語英語
ページ(範囲)1059-1062
ページ数4
ジャーナルGeophysical Research Letters
16
9
DOI
出版ステータス出版済み - 9 1989
外部発表はい

All Science Journal Classification (ASJC) codes

  • 地球物理学
  • 地球惑星科学(全般)

フィンガープリント

「The horizontally lying slab」の研究トピックを掘り下げます。これらがまとまってユニークなフィンガープリントを構成します。

引用スタイル