| Project/Area Number |
10045023
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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 | UNIVERSITY OF TSUKUBA |
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Principal Investigator |
KATO Takumi Institute of Geoscience, UNIVERSITY OF TSUKUBA Associate Professor, 地球科学系, 助教授 (90214379)
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| Co-Investigator(Kenkyū-buntansha) |
SHIMA Kunihiro Institute of Applied Physics UNIVERSITY OF TSUKUBA, 物理工学系, 助教授 (70087964)
YAGI Hisako (HIRAI,HISAKO) Institute of Geoscience, UNIVERSITY OF TSUKUBA Lecturer, 地球科学系, 講師 (60218758)
KUROSAWA Masanori Institute of Geoscience, UNIVERSITY OF TSUKUBA Lecturer, 地球科学系, 講師 (50272141)
KUBO Tomoaki Tohoku University, Graduate School of Science, 理学研究科, 助手 (40312540)
KURITA Kei University of Tokyo, Graduate School of Science, 理学系研究科, 助教授 (00111451)
末野 重穂 筑波大学, 地球科学系, 教授 (30110513)
WEIDNER Dona ニューヨーク州立大学, ストーニーブルック校, 教授
GASPARIK Tib ニューヨーク州立大学, ストーニーブルック校, 助教授
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| Project Period (FY) |
1998 – 2000
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| Project Status |
Completed (Fiscal Year 2000)
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| Budget Amount *help |
¥4,400,000 (Direct Cost: ¥4,400,000)
Fiscal Year 2000: ¥1,500,000 (Direct Cost: ¥1,500,000)
Fiscal Year 1999: ¥1,300,000 (Direct Cost: ¥1,300,000)
Fiscal Year 1998: ¥1,600,000 (Direct Cost: ¥1,600,000)
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| Keywords | Properties of the Earth's interior / High pressure phase minerals / Diamond / ICP-MS / Synchrotron X-ray |
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| Research Abstract |
This project aims to study changes of deep Earth materials and high pressure materials under high pressures.(1) Laser ablation mass spectometry has been developed to analyze trace and light elements in small area.(2) Properties of elemental carbon and related diamond materials have been studied for its industrial utilization as the hard material.(3) Nature of lithospheric mantle beneath the archean mantle has been investigated by using mantle zenolith and kimberlite magma as a prove.(4) High pressure phase transition in silicate minerals has been studied to clarify relationships between seismicity of the subduction zone and their transformation process. These studies have been made as a cooperative research with State University of New York at Stony Brook.
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