| Project/Area Number |
11440163
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| Research Category |
Grant-in-Aid for Scientific Research (B)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
Petrology/Mineralogy/Science of ore deposit
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| Research Institution | National Institute of Polar Research |
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Principal Investigator |
NOGAMI Ken-ichi Dept. of Physics, Dokkyo Univ., School of Medicine, Professor, 南極隕石研究センター, 教授 (10113896)
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| Co-Investigator(Kenkyū-buntansha) |
IMAE Naoya Antarctic Meteorite Research Center, Research Associate, 南極隕石研究センター, 助手 (60271037)
NOGUCHI Takaaki Dept. of Materials and Biological Science, Ibaraki Univ. Assoc. Professor, 理学部, 助教授 (40222195)
野上 謙一 独協医科大学, 物理学教室, 教授 (00103325)
TERADA Kentaro Dept. of Earth & Planetary System Science, Hiroshima Univ., Research Associate, 理学部, 助手 (20263668)
NAKAMURA Tomoki Earth & Planetary Science, Kyushu Univ., Assoc. Professor, 理学部, 助教授 (20260721)
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| Project Period (FY) |
1999 – 2002
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| Project Status |
Completed (Fiscal Year 2002)
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| Budget Amount *help |
¥13,900,000 (Direct Cost: ¥13,900,000)
Fiscal Year 2002: ¥2,800,000 (Direct Cost: ¥2,800,000)
Fiscal Year 2001: ¥1,800,000 (Direct Cost: ¥1,800,000)
Fiscal Year 2000: ¥2,100,000 (Direct Cost: ¥2,100,000)
Fiscal Year 1999: ¥7,200,000 (Direct Cost: ¥7,200,000)
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| Keywords | Cosmic dust / Antarctic micrometeorite / Yamato mountains / Dome Fuji / Tottuki |
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| Research Abstract |
We studied abundant Antarctic Micrometeorites collected by JARE-37, 38, 39 and 41, where JARE is Japanese Antarctic Research Expedition. Samples from JARE-37 and 38 were recovered from water tank for life in the Dome Fuji Station, those from JARE-39 from the Yamato meteorite bare icefield, and those from JARE-41 from the Tottuki bare ice area. Especially, important results were obtained from the study focused on the hydrously altered minerals. Generally, most of cosmic dust consists of hydrously altered minerals (more than 50%). On the other hand, meteorites consisting of hydrous minerals are limited to carbonaceous chondrites (〜1%). This mode of difference suggests that hydrous minerals in space fall as mostly cosmic dust, being ascribed from the fragile substance of the material. We found that recent fell Tagish Lake meteorite, which is a new type of hydrously altered carbonaceous chondrite, has a close relationship with the Antarctic micrometeorites.
In the 4th year of our research period, we summarized our study and compiled our 18 published papers, list of 41 abstracts and catalog of Japanese Antarctic Micrometeorites with more than 300 pages.
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