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平賀研究室
Showing the original Japanese · View translation
人工の岩石をつくって変形させ、地球の内部を探る研究室。
AboutAbout the lab
岩石を、原子のレベルから理解する。
平賀研究室は、
実験室で
変形実験や
地震学や
Key terms
- 多結晶
体 - 小さな
結晶の 粒が たくさん 集まって できた固体。 岩石も 多結晶体の 一つ - クリープ
- 高い
温度で 力を かけ続けた とき、 固体が ゆっくりと 変形していく 現象 - 拡散
- 原子が
物質の 中を 少し ずつ 移動していく こと。 固体が ゆっくり変形する しくみの 一つに なる
NewsLab news
View More ↗ResearchResearch themes
固体と
*Illustrative image実験用の人工の岩石をつくる
実験室で
*Illustrative image斜長石の岩石の流れにくさ
地殻の
*Illustrative imageオリビンの粒の形と結晶の向き
オリビンの
*Illustrative image粒の成長とクリープは同じしくみ
2種類の
MembersFaculty
平賀研究室の
- Professor平賀 岳彦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: “Wherlite” Strekeisen / CC BY-SA 4.0 (cropped)
- 実験用の
人工の 岩石を つくる : “Dense pellet forming9” Dominik Bejma, Marta Kowalkińska / CC BY-SA 4.0 (cropped) - 斜長石の
岩石の 流れにくさ: “Labradorescent plagioclase feldspar (Marcy Anorthosite, Mesoproterozoic, 1.16 Ga; Route 3 roadcut south of Bartlett Pond, New York State, USA) 1” James St. John / CC BY 2.0 (cropped) - オリビンの
粒の 形と 結晶の 向き: “Forsterite-Olivine-4jg58d” Robert M. Lavinsky / CC BY-SA 3.0 (cropped) - 粒の
成長と クリープは 同じしく み: “Peridotite mantle xenolith in phonotephrite (Peridot Mesa Flow, Middle Pleistocene, 580 ka; Peridot Mesa, San Carlos Volcanic Field, Arizona, USA) 26” James St. John / CC BY 2.0 (cropped) - Related lab (新谷研究室): “Interferenz-michelson” FL0 / 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 (武井研究室): “Olivine in polarizing light” Islam90 / CC BY-SA 4.0 (cropped)
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