| 固体地球科学(S) |
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| セッション小記号 | 地球内部科学・地球惑星テクトニクス |
| セッションID | S-IT25 |
| タイトル | 和文 | Deep Carbon: Diamond formation and carbon speciation in Earth and planetary processes |
| 英文 | Deep Carbon: Diamond formation and carbon speciation in Earth and planetary processes |
| タイトル短縮名 | 和文 | Deep Carbon |
| 英文 | Deep Carbon |
| 代表コンビーナ | 氏名 | 和文 | 大谷 栄治 |
| 英文 | Eiji Ohtani |
| 所属 | 和文 | 東北大学大学院理学研究科地学専攻 |
| 英文 | Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University |
| 共同コンビーナ 1 | 氏名 | 和文 | Litasov Konstantin |
| 英文 | Konstantin Litasov |
| 所属 | 和文 | V.S. Sobolev Institute of Geology and Mineralogy SB RAS |
| 英文 | V.S. Sobolev Institute of Geology and Mineralogy SB RAS |
| 共同コンビーナ 2 | 氏名 | 和文 | 鍵 裕之 |
| 英文 | Hiroyuki Kagi |
| 所属 | 和文 | 東京大学大学院理学系研究科附属地殻化学実験施設 |
| 英文 | Geochemical Research Center, Graduate School of Science, University of Tokyo |
| 共同コンビーナ 3 | 氏名 | 和文 | Craig E Manning |
| 英文 | Craig E Manning |
| 所属 | 和文 | University of California Los Angeles |
| 英文 | University of California Los Angeles |
| 発表言語 | EE |
| スコープ | 和文 | |
| 英文 | Diamonds are observed in various localities including terrestrial and extraterrestrial environments. However, there are several reports on the diamond localities from non-traditional sources including ultra-deep seated diamonds, ultrahigh pressure metamorphic rocks, various magmas, some meteorites and terrestrial craters. These diamonds might be formed by shock events, crystallization from fluids, magmas, or metallic melts, and CVD process. In this session, we welcome papers on occurrence and origin of diamonds from traditional and non-traditional sources in earth and meteorites. We also encourage the experimental studies on diamond genesis, speciation of carbon bearing compounds in terrestrial rocks and meteorites. We welcome papers on formation mechanisms of diamond in natural metal-carbon systems, chromatographic study of deep seated and experimental fluids. We also welcome papers dealing with behavior of organic materials at high pressure and high temperature corresponding to the deep earth and planets. In some chromitites, various enigmatic high pressure phases have been reported as inclusions together with diamond. We also encourage the presentations on descriptions and discussions on the origin of these materials. |
| 発表方法 | 口頭および（または）ポスターセッション |
| ジョイントセッション | AGU |
| 招待講演 | - Richard Wirth (Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences Section 4.4)
- 大藤 弘明 (愛媛大学地球深部ダイナミクス研究センター)
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