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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Early evolution of the solar accretion disk inferred from Cr-Ti-O isotopes in individual chondrules
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Early evolution of the solar accretion disk inferred from Cr-Ti-O isotopes in individual chondrules

机译:从Cr-Ti-O同位素在单个骨髓内部的Cr-Ti-O同位素推断的早期演变

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Isotopic anomalies in chondrules hold important clues about the dynamics of mixing and transport processes in the solar accretion disk. The meaning of these anomalies is debated and they have been interpreted to indicate either disk-wide transport of chondrules or local heterogeneities of chondrule precursors. However, all previous studies relied on isotopic data for a single element (either Cr, Ti, or O), which does not allow distinguishing between source and precursor signatures as the cause of the chondrules' isotope anomalies. To overcome this problem, we obtained the first combined O, Ti, and Cr isotope data for individual chondrules from enstatite, ordinary, and carbonaceous chondrites. We find that chondrules from non-carbonaceous (NC) chondrites have relatively homogeneous Lambda O-17, epsilon Ti-50, and epsilon Cr-54, which are similar to the compositions of their host chondrites. By contrast, chondrules from carbonaceous chondrites (CC) have more variable compositions, some of which differ from the host chondrite compositions. Although the compositions of the analyzed CC and NC chondrules may overlap for either epsilon Ti-50, epsilon Cr-54, or Delta O-17, in multi-isotope space, none of the CC chondrules plot in the compositional field of NC chondrites, and no NC chondrule plots within the field of CC chondrites. As such, our data reveal a fundamental isotopic difference between NC and CC chondrules, which is inconsistent with a disk-wide transport of chondrules across and between the NC and CC reservoirs. Instead, the isotopic variations among CC chondrules reflect local precursor heterogeneities, which most likely result from mixing between NC-like dust and a chemically diverse dust component that was isotopically similar to CAIs and AOAs. The same mixing processes, but on a larger, disk-wide scale, were likely responsible for establishing the distinct isotopic compositions of the NC and CC reservoirs, which represent in inner and outer disk, respectively. (C) 2020 The Author(s). Published by Elsevier B.V.
机译:软骨压力量的同位素异常对太阳能膨胀盘中的混合和运输过程的动态进行了重要的线索。这些异常的含义是讨论的,并且已经被解释为表明软骨细胞或局部多均匀性的磁盘宽传输。然而,所有先前的研究都依赖于单一元素(Cr,Ti或O)的同位素数据,其不允许区分源和前体签名作为软骨蛋白同位素异常的原因。为了克服这个问题,我们获得了来自山牙石,普通和含碳软骨的个体软骨蛋白的第一个组合O,TI和Cr同位素数据。我们发现来自非碳质(NC)的软骨细胞具有相对均匀的Lambda O-17,Epsilon Ti-50和Epsilon CR-54,其类似于其宿主细胞的组合物。相比之下,含碳软骨(CC)的软骨抑制物具有更多可变的组合物,其中一些组合物与宿主细胞内组合物不同。虽然分析的CC和NC软骨压力合物的组合物可以在多同位素空间中的epsilon Ti-50,Epsilon Cr-54或Delta O-17中重叠,但NC Chondrites的组成场中的CC软骨细胞区没有CC软骨细胞映射,在CC Chondrites领域内没有NC软骨压板。因此,我们的数据揭示了NC和CC骨髓之间的基本同位素差异,这与NC和CC水库之间的椎间盘突出的圆盘传输不一致。相反,CC软骨体中的同位素变异反映了局部前体异质性,其最有可能在与CAIS和AOA相同的同位素的不同粉尘组分之间混合。相同的混合过程,但是在较大的圆盘范围内,可能负责建立在内部和外盘中的NC和CC储存器的不同同位素组合物。 (c)2020提交人。由elsevier b.v出版。

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