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DOI | 10.1016/j.epsl.2020.116318 |
Silicon isotopic compositions of chondrule silicates in carbonaceous chondrites and the formation of primordial solids in the accretion disk | |
Villeneuve J.; Marrocchi Y.; Jacquet E. | |
发表日期 | 2020 |
ISSN | 0012821X |
卷号 | 542 |
英文摘要 | We determined the silicon isotopic compositions of silicates (olivine and low-Ca pyroxene) in type I and type II chondrules of the carbonaceous chondrites Allende, Kaba, NWA (Northwest Africa) 5958, and MIL (Miller Range) 07342. Type I chondrule silicates show large, mass-dependent Si isotopic fractionations, with δ30Si values ranging from −7‰ to +2.6‰, whereas the δ30Si values of type II chondrule silicates are close to zero and vary by less than 2‰. When present, Mg-rich relict olivine grains in type II chondrules show larger Si variations than their FeO-rich counterparts. In type I chondrules, low-Ca pyroxenes yield systematically lighter δ30Si values than Mg-rich olivines. Our results show that type I chondrules are complex objects whose Si isotopic compositions derived from their precursors and SiO-rich gas-melt interactions. This corroborates that type I chondrules are nebular products that formed under open-system conditions. Our data also suggest that at least some type II chondrules derived from their type I counterparts. Overall, this demonstrates that recycling was common during the evolution of the protoplanetary disk. © 2020 Elsevier B.V. |
关键词 | carbonaceous chondriteschondrulesion probesilicon isotopessolar system formation |
英文关键词 | Iron oxides; Isotopes; Magnesium compounds; Meteorites; Olivine; Silicates; Silicon oxides; Accretion disks; Carbonaceous chondrites; Complex objects; FeO-rich; Isotopic composition; Isotopic fractionations; Protoplanetary disks; System conditions; Calcium compounds; chondrite; chondrule; isotopic composition; isotopic fractionation; olivine; silicate; silicon |
语种 | 英语 |
来源期刊 | Earth and Planetary Science Letters |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/202948 |
作者单位 | CRPG, CNRS, Université de Lorraine, UMR 7358, Vandœuvre-lès-Nancy, 54501, France; Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie (IMPMC), Muséum national d'Histoire naturelle, Sorbonne Université, CNRS, CP52, 57 rue Cuvier, Paris, 75005, France |
推荐引用方式 GB/T 7714 | Villeneuve J.,Marrocchi Y.,Jacquet E.. Silicon isotopic compositions of chondrule silicates in carbonaceous chondrites and the formation of primordial solids in the accretion disk[J],2020,542. |
APA | Villeneuve J.,Marrocchi Y.,&Jacquet E..(2020).Silicon isotopic compositions of chondrule silicates in carbonaceous chondrites and the formation of primordial solids in the accretion disk.Earth and Planetary Science Letters,542. |
MLA | Villeneuve J.,et al."Silicon isotopic compositions of chondrule silicates in carbonaceous chondrites and the formation of primordial solids in the accretion disk".Earth and Planetary Science Letters 542(2020). |
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