2012 Fiscal Year Final Research Report
Experimental determination of carbon isotope fractionation in theFe-C system under HPHT conditions.
Project/Area Number |
23654186
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Research Category |
Grant-in-Aid for Challenging Exploratory Research
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Allocation Type | Multi-year Fund |
Research Field |
Petrology/Mineralogy/Science of ore deposit
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Research Institution | Niigata University (2012) Shizuoka University (2011) |
Principal Investigator |
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Co-Investigator(Kenkyū-buntansha) |
YOSHINO Takashi 岡山大学, 地球物質科学研究センター, 准教授 (30423338)
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Project Period (FY) |
2011 – 2012
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Keywords | 岩石 / 鉱物 / 鉱床学 / 炭素同位体 / Fe-C系 / 高温高圧実験 / 同位体分別 |
Research Abstract |
Equilibrium carbon isotope fractionation between graphite/diamond and iron carbide melt at 5 and 10 GPa and in the temperature range between 1200 and 2000 oC was determined. The results suggest that iron carbide melt will preferentially accumulate12^C rather than 13^C. We proposed that the temperature-dependent fractionation of carbon isotopes between iron carbide melt and graphite/diamond might have created a “12^C-enriched core” with a significant difference in the distribution of carbon isotopes between the carbon in the metallic core and bulk silicate Earth during the accretion and differentiation of early Earth.
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[Presentation] Understanding carbon isotopesystematics in the deep Earth2012
Author(s)
Satish-Kumar, M., Yoshino, T., Mizutani, S., So, H., Kato, M.
Organizer
Joint Symposium of Misasa-2012 and Geofluid-2: Dynamics and Evolution of the Earth's Interior: special emphasis on the role of fluids
Place of Presentation
Institute for Study of the Earth's Interior,Okayama University, Misasa, apan(招待講演)
Year and Date
20120318-21
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