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宇野研究室(Uno Lab)
Showing the original Japanese · View translation
岩石と流体の反応から地球内部の変動を探る研究室。
AboutAbout the lab
岩石と流体の反応から、地球の中を読み解く。
宇野研究室は、
地震発生帯の
野外地質調査、
地球内部の
Key terms
- 流体
- 水や
ガスのように 流れる 性質を もつ物質。 地下では 岩石の すき間を 動き、 岩石と 反応する - 鉱物炭酸塩化
- 岩石の
中の 鉱物が 二酸化炭素と 反応して、 炭酸塩鉱物に 変わる こと - 超臨界
- 高い
温度と 圧力のもとで、 液体とも気体とも 区別できなくなった 状態 - 変成帯
- 地下の
高い 温度や 圧力を 受けて、 岩石が つくり変えられた 地域
ResearchResearch themes
沈み込み帯の
*Illustrative imageマグマ性流体による地殻破壊
東南極セール・ロンダーネ山地の
*Illustrative image鉱物炭酸塩化
高温高圧の
*Illustrative image地震発生帯の岩石学
三波川変成帯の
*Illustrative image超臨界地熱
超
MembersFaculty
宇野研究室の
- Associate Professor宇野 正起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: “Big garnet amphibolite (Precambrian; Warrensburg, Adirondack Mountains, New York State, USA) 26” James St. John / CC BY 2.0 (cropped)
- マグマ性流体に
よる 地殻破壊: “Satellite image of Sør Rondane Mountains, Antarctica ( ) (cropped)” NASA Goddard Space Flight Center from Greenbelt, MD, USA / Public domain (cropped) - 鉱物炭酸塩化: “Liswanite” Diorit / CC0 (cropped)
- 地震発生帯の
岩石学: “Nagatoro Iwadatami Rocks ( )” Guilhem Vellut from Annecy, France / CC BY 2.0 (cropped) - 超
臨界地熱: “Krafla” Hansueli Krapf / CC BY-SA 3.0 (cropped) - Related lab (瀧川研究室): “Allende meteorite ( )” Steve Jurvetson / CC BY 2.0 (cropped)
- Related lab (鈴木庸平研究室): “BlackSmoker” W.R. Normark, Dudley Foster / Public domain (cropped)
- Related lab (分子地球化学研究室
（MGL） ): “Diamond by Peter Smyth” Peter Smyth / CC0 (cropped) - Related lab (板井研究室): “LakeBiwa” Ka23 13 / CC BY-SA 4.0 (cropped)
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