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亀研究室(地震破壊理論)
Showing the original Japanese · View translation
地震がなぜ複雑に起こるのかを、理論とシミュレーションで解き明かす研究室。
AboutAbout the lab
紙と鉛筆と計算機で、地震の起こり方に迫る。
亀研究室は、
地震の
実験室では
観測データと
Key terms
- データ同化
- 観測データを
数値モデルに 取り込み、 モデルの 状態や 将来の 予測を 修正していく 手法。 天気予報で 使われている - スロースリップ
- プレートの
境界が、 揺れを 出さずに 数日から 数年かけて ゆっくりすべる 現象 - 動的破壊
- 断層が
高速で 壊れていく 過程。 破壊が 断層面を 広がりながら地震波を 出す
NewsLab news
View More ↗ResearchResearch themes
実験では
*Illustrative image断層の複雑な破壊の動き
地震の
*Illustrative image巨大地震の繰り返しのシミュレーション
プレートの
*Illustrative image重力の変化で地震をいち早く検出
断層の
*Illustrative image不均質な地殻の中での地震破壊
地震破壊の
MembersFaculty
亀研究室の
- Professor亀 伸樹Publications ↗
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Report an errorAbout the images
The top and research theme images are illustrative and were not taken at the lab. They are cropped from Wikimedia Commons images. Cropped CC BY-SA images are provided under the same CC BY-SA license as the original (version shown on each line).
- Top image: “Fault Scarp Borah Peak Earthquake 1983” R.E. Wallace, USGS Earthquake Information Bulletin 501 / Public domain (cropped)
- 断層の
複雑な 破壊の 動き: “Kamishiro fault earthquake 6” Apple2000 / CC0 (cropped) - 巨大地震の
繰り返しの シミュレーション: “Earthquake cycle for megathrust earthquake” Xiaohan Song / CC BY-SA 4.0 (cropped) - 重力の
変化で 地震を いち早く 検出: “In-construction KAGRA gravitational-wave detector” Christopher Berry / CC BY-SA 4.0 (cropped) - 不均質な
地殻の 中での 地震破壊: “Outcrop of Kannawa Fault near Minase River” Azegamaru / CC BY 4.0 (cropped)
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