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加藤愛太郎研究室
Showing the original Japanese · View translation
地震観測のデータから、地震がどう始まるかを探る研究室。
AboutAbout the lab
地震は、どのようにして始まるのか。
加藤研究室は、
断層が
大きな
Key terms
- スロースリップ
- 断層が
ふつうの 地震よりも ゆっくりずれ動いて、 たまった ひずみの エネルギーを 解き放つ現象 - 前震
- 大きな
地震 （本震）の 前に、 その 近くで 起きる 地震 - 低周波地震
- ふつうの
地震に 比べて、 ゆっくりした 揺れが 目立つ 小さな 地震 - 群発地震
- は
っきりした 本震が 無く、 ある 地域で 地震が 続けて 起きる 現象
ResearchResearch themes
地震が
*Illustrative image大地震はどう始まるか
大地震の
*Illustrative image高密度の地震観測で見る断層
2000年鳥取県西部地震の
*Illustrative image低周波地震とすべりの移り変わり
プレート境界の
*Illustrative image余震や群発地震の仕組み
余震や
MembersFaculty
加藤研究室の
- Professor加藤 愛太郎Publications ↗
VoicesStudent voices
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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: “Japan earthquake map” Jackopoid / CC BY-SA 3.0 (cropped)
- 大地震は
どう 始まる か : “Kumamoto Earthquake, Japan (ASTER)” NASA/METI/AIST/Japan Space Systems, and U.S./Japan ASTER Science Team / Public domain (cropped) - 高密度の
地震観測で 見る断層: “CMG-40T Triaxial Broadband Seismometer” Z22 / CC BY-SA 3.0 (cropped) - 低周波地震と
すべりの 移り 変わり: “Nankai trough topographic” Peka / CC BY-SA 3.0 (cropped) - 余震や
群発地震の 仕組み: “Seismogram at Weston Observatory” Z22 / CC BY-SA 3.0 (cropped) - Related lab (望月研究室
（海域地震学） ): “Test des sismomètres OBS (Ocean Bottom Seismometer) en bassin d'essais (Ifremer )” Olivier Dugornay (Ifremer) / CC BY 4.0 (cropped) - Related lab (中谷研究室): “Fault slickenside (Great Smoky Mountains, Tennessee-North Carolina, USA) 1” James St. John / CC BY 2.0 (cropped)
- Related lab (三宅研究室(地震研 地震火山災害部門)): “Aso house damaged by the 2016 Kumamoto earthquake 2” hanonimas / CC BY-SA 3.0 (cropped)
- Related lab (綿田研究室(地球惑星ダイナミクス)): “SWOT Satellite Measures Pacific Tsunami (PIA26652)” NASA/JPL-Caltech / Public domain (cropped)
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