2000年鳥取県西部地震 (<i>M</i><sub>J</sub>=7.3) に先行した震源分布のフラクタル次元の特徴的変化

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タイトル別名
  • The Characteristic Changes in Fractal Dimension Preceding the 2000 Tottori-ken Seibu Earthquake (<i>M</i><sub>J</sub>=7.3)
  • 2000年鳥取県西部地震(MJ=7.3)に先行した震源分布のフラクタル次元の特徴的変化
  • 2000ネン トットリケン セイブ ジシン MJ 7 3 ニ センコウ シタ シンゲン ブンプ ノ フラクタルジゲン ノ トクチョウテキ ヘンカ

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The author investigated fractal structure of hypocentral distributions before the 2000 Tottoriken Seibu earthquake (MJ=7.3), by estimating temporal changes in the spatial fractal dimension D of the hypocenter distributions, and comparing these results with the seismic activity in and around the focal region. The correlation integral method and the running time-window technique were applied to the D-value calculation for the JMA Earthquake Catalogue data during the period of January 1983 -February 2001. The results obtained are summarized as follows; (1) The D-value decreased drastically prior to the main shock in and around the focal region. The precursory durations are estimated as 1-3 years, which may be different with different sizes of the time-window. (2) The D-value decrease must be caused by hypocenter clusterings, or unusual seismic activity, which occurred over the wide area in and around the focal region. (3) Consequently, temporal variations in the D-values associated with a large earthquake may be effective as a precursor to the earthquake.

収録刊行物

  • 地震 第2輯

    地震 第2輯 55 (1), 11-18, 2002

    公益社団法人 日本地震学会

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