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DOI | 10.1038/s41561-018-0128-2 |
Oxidized conditions in iron meteorite parent bodies | |
Bonnand, P.1,2; Halliday, A. N.1,3 | |
2018-06-01 | |
发表期刊 | NATURE GEOSCIENCE
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ISSN | 1752-0894 |
EISSN | 1752-0908 |
出版年 | 2018 |
卷号 | 11期号:6页码:401-+ |
文章类型 | Article |
语种 | 英语 |
国家 | England; France; USA |
英文摘要 | Magmatic iron meteorites are thought to originate from the cores of differentiated planetary embryos, but it is unclear where they formed in the circumstellar disk. Oxygen fugacity (fO(2)) is thought to have varied radially across the disk, affecting planetary accretion and core formation. Metal-silicate equilibration experiments show that the chromium concentration in metallic melt increases with decreasing fO(2). Chromium can therefore be used to reconstruct fO(2) during metal segregation. Here, we report mass-dependent fractionation of stable chromium isotopes measured for several groups of magmatic iron meteorites. We find that chromium concentrations are variable and most samples are isotopically heavy compared with the bulk silicate Earth and chondrites. Although it is evident that the chromium isotopes were systematically affected by fractional crystallization, we use the mass-dependent fractionation behaviour to derive initial chromium concentrations for the planetary embryo cores. We find that the cores were diverse in fO(2) and demonstrate that core formation in some planetary embryos occurred under relatively oxidizing conditions (fO(2) relative to iron-wustite (IW) buffer (Delta IW) = -0.95 +/- 0.15). It is difficult to reconcile this with the view that iron meteorite parent bodies formed closer to Earth and subsequently migrated outwards. Instead, we suggest that these parent bodies formed at greater distances, beyond Mars. |
领域 | 地球科学 ; 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000433901600011 |
WOS关键词 | CHROMIUM ISOTOPIC COMPOSITION ; MASS-DEPENDENT FRACTIONATION ; OXIDATION-STATE ; CORE FORMATION ; CR ; EARTH ; METAL ; CHONDRITES ; MANTLE ; CRYSTALLIZATION |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/34928 |
专题 | 地球科学 气候变化 |
作者单位 | 1.Univ Oxford, Dept Earth Sci, Oxford, England; 2.Univ Clermont Auvergne, CNRS, Lab Magmas & Volcans, Clermont Ferrand, France; 3.Columbia Univ, Earth Inst, New York, NY USA |
推荐引用方式 GB/T 7714 | Bonnand, P.,Halliday, A. N.. Oxidized conditions in iron meteorite parent bodies[J]. NATURE GEOSCIENCE,2018,11(6):401-+. |
APA | Bonnand, P.,&Halliday, A. N..(2018).Oxidized conditions in iron meteorite parent bodies.NATURE GEOSCIENCE,11(6),401-+. |
MLA | Bonnand, P.,et al."Oxidized conditions in iron meteorite parent bodies".NATURE GEOSCIENCE 11.6(2018):401-+. |
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