Nanoparticles in natural beryllium-bearing sapphire: incorporation and exsolution of high field strength elements in corundum

IF 3.5 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Contributions to Mineralogy and Petrology Pub Date : 2024-11-28 DOI:10.1007/s00410-024-02189-y
Shiyun Jin, David W. Saxey, Zakaria Quadir, Steven M. Reddy, William D. A. Rickard, Denis Fougerouse, Xiao Sun, Aaron C. Palke
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Abstract

In natural corundum, a strong geochemical correlation is sometimes observed between Be and heavy high field strength elements (HHFSEs) such as Nb, Ta and W, and it has been hypothesized that trace elements are hosted in primary inclusions. However, no known mineral enriched in both Be and HHFSEs stable at these geological conditions can explain this correlation. To understand how Be and HHFSEs are distributed in natural corundum down to the atomic scale, two natural Be-bearing sapphire crystals from Afghanistan and Nigeria are studied using laser ablation inductively coupled plasma and time-of-flights secondary ion mass spectrometry, atom probe tomography and transmission electron microscopy. In addition to common trace elements such as Mg, Ti, and Fe, Be and W are detected in the metamorphic sapphire from Afghanistan, whereas Be, Nb and Ta are detected in the magmatic sapphire from Nigeria. Nanoclustering in both samples shows fractionation of Be and high field strength elements (including Ti) by atomic mass, suggesting a secondary process controlled by solid-state diffusion. The homogeneously distributed W and the secondary nano-precipitates bearing Nb and Ta indicates that HHFSEs can be incorporated into the corundum structure during crystallization, most likely through preferred adsorption on the growth surface. The strong correlation between Be and HHFSEs across the growth zones is probably due to Be being attracted by HHFSEs to partially balance the charge when incorporated into the corundum structure. The enrichment of high field strength elements by growth kinetics may result in supersaturated concentrations during crystallization, allowing them to precipitate out when the host corundum is heated above its formation temperature by basaltic magma. Comparison with previous transmission electron microscope studies suggests the same process for incorporating Be and HHFSEs also applies to other natural corundums from different localities.

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天然含铍蓝宝石中的纳米颗粒:高场强元素在刚玉中的掺入和排出
在天然刚玉中,有时会观察到 Be 与 Nb、Ta 和 W 等重型高场强元素(HHFSE)之间存在很强的地球化学相关性,因此有人推测微量元素寄存在原生包裹体中。然而,在这些地质条件下,没有一种已知的富含 Be 和 HHFSE 的矿物能够解释这种相关性。为了了解铍和 HHFSE 如何在天然刚玉中以原子尺度分布,我们使用激光烧蚀电感耦合等离子体和飞行时间二次离子质谱、原子探针断层扫描和透射电子显微镜对阿富汗和尼日利亚的两块天然含铍蓝宝石晶体进行了研究。除 Mg、Ti 和 Fe 等常见痕量元素外,在阿富汗的变质蓝宝石中还检测到 Be 和 W,而在尼日利亚的岩浆蓝宝石中则检测到 Be、Nb 和 Ta。这两种样品中的纳米聚类显示了 Be 和高场强元素(包括 Ti)按原子质量的分馏,表明这是一个由固态扩散控制的次生过程。均匀分布的 W 以及含有 Nb 和 Ta 的次生纳米沉淀物表明,高场强元素可以在结晶过程中融入刚玉结构,很可能是通过生长表面的优先吸附作用。Be 和 HHFSEs 在整个生长区之间的强相关性可能是由于 Be 被 HHFSEs 吸引,从而在融入刚玉结构时部分平衡了电荷。生长动力学对高场强元素的富集可能会导致结晶过程中的过饱和浓度,使其在玄武岩浆将主刚玉加热到高于其形成温度时析出。与之前的透射电子显微镜研究比较表明,掺入铍和高场强元素的过程同样适用于来自不同地区的其他天然刚玉。
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来源期刊
Contributions to Mineralogy and Petrology
Contributions to Mineralogy and Petrology 地学-地球化学与地球物理
CiteScore
6.50
自引率
5.70%
发文量
94
审稿时长
1.7 months
期刊介绍: Contributions to Mineralogy and Petrology is an international journal that accepts high quality research papers in the fields of igneous and metamorphic petrology, geochemistry and mineralogy. Topics of interest include: major element, trace element and isotope geochemistry, geochronology, experimental petrology, igneous and metamorphic petrology, mineralogy, major and trace element mineral chemistry and thermodynamic modeling of petrologic and geochemical processes.
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