首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Oxygen isotopic constraints on the origin and parent bodies of eucrites, diogenites, and howardites
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Oxygen isotopic constraints on the origin and parent bodies of eucrites, diogenites, and howardites

机译:氧同位素限制了欧氏体,双辉石和芒硝的来源和母体

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摘要

A few eucrites have anomalous oxygen isotopic compositions. To help understand their origin and identify additional samples,we have analyzed the oxygen isotopic compositions of 18 eucrites and four diogenites. Except for five eucrites, these meteorites have D17O values that lie within 2r of their mean value viz., 0.242 ± 0.016&, consistent with igneous isotopic homogenization of Vesta. The five exceptional eucrites—NWA 1240, Pasamonte (both clast and matrix samples), PCA 91007, A-881394, and Ibitira—have D17O values that lie, respectively, 4r, 5r, 5r, 15r, and 21r away from this mean value.NWA 1240 has a d18O value that is 5r below the mean eucrite value. Four of the five outliers are unbrecciated and unshocked basaltic eucrites, like NWA 011, the first eucrite found to have an anomalous oxygen isotopic composition. The fifth outlier,Pasamonte, is composed almost entirely of unequilibrated basaltic clasts. Published chemical data for the six eucrites with anomalous oxygen isotopic compositions (including NWA 011) exclude contamination by chondritic projectiles as a source of the oxygen anomalies. Only NWA 011 has an anomalous Fe/Mn ratio, but several anomalous eucrites have exceptional Na, Ti, or Cr concentrations. We infer that the six anomalous eucrites are probably derived from five distinct Vesta-like parent bodies (Pasamonte and PCA 91007 could come from one body). These anomalous eucrites, like the isotopically normal,unbrecciated eucrites with 4.48 Gyr Ar-Ar ages, are probably deficient in brecciation and shock effects because they were sequestered in small asteroids (10 km diameter) during the Late Heavy Bombardment following ejection from Vesta-like bodies. The preservation of Vesta’s crust and the lack of deeply buried samples from the hypothesized Vesta-like bodies are consistent with the removal of these bodies from the asteroid belt by gravitational perturbations from planets and protoplanets,rather than by collisional grinding.
机译:少数玉质具有异常的氧同位素组成。为了帮助了解它们的起源并确定其他样品,我们分析了18个碳酸盐岩和4个重辉石的氧同位素组成。除了五种陨石外,这些陨石的D17O值均在其平均值的2r之内,即0.242±0.016&,这与Vesta的火成岩同位素均质一致。 NWA 1240,Pasamonte(包括碎屑样品和基质样品),PCA 91007,A-881394和Ibitira这5种出色的eucrites的D17O值分别偏离该平均值4r,5r,5r,15r和21r。 .NWA 1240的d18O值比平均eucrite值低5r。五个离群值中的四个是未结块且不受冲击的玄武质玉石,例如NWA 011,这是第一个发现的氧同位素组成异常的玉石。第五个异常点,Pasamonte,几乎完全由未平衡的玄武岩碎屑组成。已发布的六种具有异常氧同位素组成的玉石的化学数据(包括NWA 011)排除了作为氧异常来源的软骨球质弹丸的污染。只有NWA 011的Fe / Mn比值异常,但是几种异常的eucrites具有异常的Na,Ti或Cr浓度。我们推断这六个异常的欧亚岩可能来自五个不同的类似维斯塔的母体(Pasamonte和PCA 91007可能来自一个体)。这些异常的欧氏体,如同位素年龄为4.48 Gyr Ar-Ar的正常未结冰质的欧氏体,可能在缩微作用和冲击作用方面缺乏,因为它们在重质轰炸后期从维斯塔式的弹射中被隔离在小行星(直径10 km)中身体。维斯塔地壳的保存以及假想的维斯塔样体缺乏深埋的样品,与通过行星和原行星的引力扰动而不是通过碰撞研磨将这些天体从小行星带中移除相一致。

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