Search for pre-accretionary irradiation effects in calcium-aluminum inclusions from the CV3 chondrite Allende

IF 2.2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
P. Ghaznavi, C. Burkhardt, F. L. H. Tissot, I. Leya
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引用次数: 0

Abstract

Calcium-aluminum-rich inclusions (CAIs) are the first objects that formed in the solar accretion disk and therefore provide valuable insights into the evolution of the early solar system. A long-standing question regarding this earliest formative period relates to the storage of CAIs in the 1–4 Myr time period between their formation and later accretion into chondrite parent bodies. Were the CAIs stored in a pre-existing parent body, or in distant parts of the solar accretion disk? In the latter scenario, CAIs might have been exposed to cosmic rays, either from the galaxy or from the Sun and such pre-accretion irradiation effects might be detectable. We searched for such pre-accretional irradiation effects in 7 fine- and 11 coarse-grained CAIs from the CV 3.6 carbonaceous chondrite Allende. The extracted samples were analyzed for their major chemical composition and all samples were analyzed using μCT techniques. Using physical model calculations, 21Necos and (22Ne/21Ne)cos production rate ratios were calculated for each CAI by fully considering their individual chemical composition. Measured He, Ne, Ar, and Kr isotope compositions of the CAIs show cosmogenic signals; clear signals for He and Ne isotopes; and detectable signals for some of the Ar and Kr isotopes. In addition, most samples show clear indications for radiogenic 4He and some samples show evidence for radiogenic 40Ar. Higher 36Ar/38Ar, 22Ne/21Ne, 80Kr/84Kr, and 82Kr/84Kr ratios together with lower cosmogenic 38Arcos concentrations in fine-grained CAIs compared to coarse-grained CAIs are consistent with more alteration of the former compared to the latter. The CRE ages for the CAIs range between 4.12 ± 0.41 Myr and 6.40 ± 0.63 Myr. Statistical tests indicate that the data are normally distributed with no outliers, indicating that all CAIs share a common irradiation history, likely the irradiation in the Allende meteoroid. The average CRE age of 4.87 ± 0.19 Myr agrees with the nominally accepted CRE age of Allende of ~5.2 Myr. There is no correlation between 21Necos concentrations and indicators of aqueous alteration like Na and/or U concentrations. The lack of correlation together with the finding of normally distributed modeled CRE ages indicates that either none of the studied CAIs experienced a pre-accretion irradiation before parent body compaction and/or that any pre-accretion irradiation effects have been completely erased during aqueous alteration events. Taking alteration aside, the findings are not in favor of X-wind type models but are more consistent with the idea of CAI outward transport in an expanding disk.

Abstract Image

寻找来自CV3球粒陨石Allende的钙铝包裹体的增生前辐射效应
富钙铝包裹体(CAIs)是在太阳吸积盘中形成的第一批物体,因此为早期太阳系的演化提供了有价值的见解。关于这一最早形成时期的一个长期存在的问题涉及到cai在其形成和后来积聚到球粒陨石母体之间的1 - 4myr时间内的储存。cai是储存在一个先前存在的母体中,还是储存在太阳吸积盘的遥远部分?在后一种情况下,cai可能已经暴露在来自银河系或太阳的宇宙射线中,这种吸积前的辐射效应可能是可以探测到的。我们在CV 3.6碳质球粒陨石Allende的7个细粒和11个粗粒CAIs中寻找了这种增生前辐射效应。对提取的样品进行主要化学成分分析,并用μCT技术对所有样品进行分析。通过物理模型计算,充分考虑每种CAI的化学成分,计算出每种CAI的21Necos和(22Ne/21Ne)cos产率比。CAIs的He、Ne、Ar、Kr同位素组成显示宇宙成因信号;He和Ne同位素信号清晰;以及某些Ar和Kr同位素的可探测信号。此外,大多数样品显示放射成因4He的明显迹象,一些样品显示放射成因40Ar的证据。细粒CAIs 36Ar/38Ar、22Ne/21Ne、80Kr/84Kr和82Kr/84Kr比值高于粗粒CAIs,宇宙成因38Arcos浓度低于粗粒CAIs,说明细粒CAIs的蚀变大于粗粒CAIs。CRE年龄在4.12±0.41 Myr ~ 6.40±0.63 Myr之间。统计检验表明,数据呈正态分布,无异常值,表明所有cai具有共同的辐照历史,可能是Allende流星体的辐照。平均CRE年龄为4.87±0.19 Myr,与Allende名义上接受的~5.2 Myr的CRE年龄一致。21Necos浓度与Na和/或U浓度等水性蚀变指标之间没有相关性。缺乏相关性以及正态分布的模拟CRE年龄的发现表明,所研究的CAIs在母体压实之前没有经历过预吸积辐射,或者在水蚀变事件中任何预吸积辐射效应都被完全消除了。撇开改变不谈,这些发现并不支持x风型模型,而更符合CAI在膨胀盘中向外输运的观点。
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来源期刊
Meteoritics & Planetary Science
Meteoritics & Planetary Science 地学天文-地球化学与地球物理
CiteScore
3.90
自引率
31.80%
发文量
121
审稿时长
3 months
期刊介绍: First issued in 1953, the journal publishes research articles describing the latest results of new studies, invited reviews of major topics in planetary science, editorials on issues of current interest in the field, and book reviews. The publications are original, not considered for publication elsewhere, and undergo peer-review. The topics include the origin and history of the solar system, planets and natural satellites, interplanetary dust and interstellar medium, lunar samples, meteors, and meteorites, asteroids, comets, craters, and tektites. Our authors and editors are professional scientists representing numerous disciplines, including astronomy, astrophysics, physics, geophysics, chemistry, isotope geochemistry, mineralogy, earth science, geology, and biology. MAPS has subscribers in over 40 countries. Fifty percent of MAPS'' readers are based outside the USA. The journal is available in hard copy and online.
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