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石川研究室
Showing the original Japanese · View translation
深部マントルの岩石から、固体地球の歴史を精密に読み解く研究室。
AboutAbout the lab
固体地球進化史の精密解読
石川研究室は、
手が
中でも、
Key terms
- マントル
- 地球の
表面の 地殻の 下、 中心の 核の 外側に ある 厚い 岩石の 層 - テクトニクス
- 地球の
表面を おおう岩盤の 動きなど、 大地を 動かし 形づくるしく み - 太古代
- 地球の
歴史の 前半に あたる、 はるか昔の 地質時代。 その 終わり ごろに 地球の 表面に 酸素が たまり 始めた - 顕生代
- 目に
見える 大きさの 生き物の 化石が 数多く 見つかるようになってから、 現在までの 時代
ResearchResearch themes
天然の
*Illustrative image生まれたばかりの地球
世界に
*Illustrative image現在のマントル
地球の
*Illustrative image顕生代の大量絶滅
大量絶滅と
*Illustrative image地球史最大の転換点
地球の
MembersFaculty
石川研究室の
- Associate Professor石川 晃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: “Lherzolite mantle xenolith in basalt (Afton Basalt Flow Upper Pleistocene, 15-20 ka; Kilbourne Hole Crater, Aden-Afton Basalt Field, Potrillo Volcanic Field, southwestern New Mexico, USA) ( )” James St. John / CC BY 2.0 (cropped)
- 生まれた
ばかりの 地球: “Acasta Gneiss from Canada” James St. John / CC BY 2.0 (cropped) - 現在の
マントル: “Spinel lherzolite - Neoproterozoic-aged xenolith in Pleistocene basalt (Mt. Leura Complex, Newer Volcanics Province; Mt. Leura, southwestern Victoria, southeastern Australia) ( )” James St. John / CC BY 2.0 (cropped) - 顕生代の
大量絶滅: “K–Pg boundary in Colorado” Jeffrey Beall / CC BY 4.0 (cropped) - 地球史最大の
転換点: “Tiger Iron2” James St. John / CC BY 2.0 (cropped) - Related lab (尾﨑研究室): “Blue Marble Western Hemisphere” NASA / Reto Stöckli / Public domain (cropped)
- Related lab (上野雄一郎研究室): “Stromatolites at Hamelin Pool in Shark Bay - Western Australia - 27 Aug. 2014” Bryn Pinzgauer / CC BY 2.0 (cropped)
- Related lab (中島研究室): “A seismogram of 2011 Tōhoku earthquake and tsunami” Z22 / CC BY-SA 3.0 (cropped)
- Related lab (癸生川研究室): “Carbonaceous chondrite (Murchison Meteorite) ( )” James St. John / CC BY 2.0 (cropped)
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