Transportation process of transitional-metal elements by fluid and/or melt in the upper mantle beneath the arc
Project/Area Number |
21740375
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Research Category |
Grant-in-Aid for Young Scientists (B)
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Allocation Type | Single-year Grants |
Research Field |
Petrology/Mineralogy/Science of ore deposit
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Research Institution | Kumamoto University (2011) Kanazawa University (2009-2010) |
Principal Investigator |
ISHIMARU Satoko 熊本大学, 大学院・自然科学研究科, 助教 (60464046)
|
Research Collaborator |
ARAI Shoji 金沢大学, 大学院・自然科学研究科, 教授 (20107684)
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Project Period (FY) |
2009 – 2011
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Project Status |
Completed (Fiscal Year 2011)
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Budget Amount *help |
¥4,420,000 (Direct Cost: ¥3,400,000、Indirect Cost: ¥1,020,000)
Fiscal Year 2011: ¥1,040,000 (Direct Cost: ¥800,000、Indirect Cost: ¥240,000)
Fiscal Year 2010: ¥1,170,000 (Direct Cost: ¥900,000、Indirect Cost: ¥270,000)
Fiscal Year 2009: ¥2,210,000 (Direct Cost: ¥1,700,000、Indirect Cost: ¥510,000)
|
Keywords | マントル / 地球化学 / 沈み込み帯 / 交代作用 / 島弧 / 岩石・鉱物・鉱床 / 地殻・マントル物質 |
Research Abstract |
We examined two different types of mantle-derived peridotites to clarify modification processes, especially to transportation of transitional-metal elements, by melts or slab-derived fluids : the one is xenoliths from sub-arc mantle beneath the volcanic front and the other is solid intrusive peridotite blocks and peridotites at the bottom of Oman ophiolite. Then, we identified that the sub-arc mantle beneath the volcanic front is highly metasomatized and some elements(e. g., Ni, Fe and platinum-group elements) are partly concentrated in there. In addition, we found H_2O-bearing inclusions in sub-arc mantle xenoliths. However there have been quite a few reports of H_2O inclusions even in arc-derived materials, we confirmed that H_2O is the main fluid phase within the sub-arc upper mantle beneath the volcanic front.
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Report
(4 results)
Research Products
(45 results)
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[Journal Article] Chemical characteristics of chromian spinel in plutonic rocks : implications for deep magma processes and discrimination of tectonic setting2011
Author(s)
Arai, S., Okamura, H., Kadoshima, K., Tanaka, C., Suzuki, K. and Ishimaru, S
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Journal Title
Island Arc
Volume: 20
Pages: 125-137
NAID
Related Report
Peer Reviewed
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[Journal Article] Chemical characteristics of chromian spinel in plutonic rocks : Implications for deep magma processes and discrimination of tectonic setting2011
Author(s)
Arai, S., Okamura, H., Kadoshima, K., Tanaka, C., Suzuki, K., Ishimaru, S.
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Journal Title
Journal of Mineralogical and Petrological Sciences
Volume: 20(1)
Pages: 125-137
NAID
Related Report
Peer Reviewed
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[Journal Article] Rock seismic anisotropy of the low-velocity zone beneath the volcanic front in the mantle wedge2009
Author(s)
Michibayashi, K., Oohara, T., Satsukawa, T., Ishimaru, S., Arai, S. and Okrugin, V. M.
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Journal Title
Geophysical Research Letters
Volume: 36
Issue: 12
DOI
NAID
Related Report
Peer Reviewed
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[Journal Article] Unusual ultra-depleted dunite from Sibuyan Island (the Philippines) : a residue for ultra-depleted MORB?2009
Author(s)
Payot, B.D., Arai, S., Tamura, A., Ishimaru, S., Tamayo, Jr., R.A.
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Journal Title
Journal of Mineralogical and Petrological Sciences 104
Pages: 383-388
NAID
Related Report
Peer Reviewed
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