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3D nanopetrography and chemical imaging of datable zircons by synchrotron multimodal X-ray tomography

机译:Synchrotron多模式X射线断层扫描的3D纳米甲型和化学成像通过同步氧化锆

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Zircon is the most widely used mineral in petrochronology and provides key information about magmatic and crustal differentiation history of plutonic rocks, transport paths of clastic material ‘from source to sink’ and significantly contributes in the reconstruction of enigmatic planetary-scale tectonic episodes since the Archaean. However, detailed textural analysis of this accessory mineral has always been hampered by two-dimensional (2D) analytical limitations. With the advancements in X-ray nanotomography technology, it is now possible to non-destructively, yet digitally, cut, visualize, compare and quantify internal textures within zircons, their growth and zoning patterns and chemical distribution of trace elements in three dimensions (3D). We present a novel multimodal approach of using a synchrotron radiation nanobeam to perform 3D nanopetrography of ?100?μm zircons at ~100?nm resolution, demonstrating the capabilities of the technique by analysis of Paleoproterozoic zircons from the Central Finland Granitoid Complex. The integrated X-ray absorption, diffraction and fluorescence tomography revealed sector and oscillatory zoning patterns in 3D as well as differences in zoning pattern between trace elements, in addition to lattice parameters and inclusion composition within zircons. The multimodal synchrotron nanotomography elucidates the 3D nanopetrography and trace element composition of submillimeter-sized zircons in unprecedented detail.
机译:锆石是卓越的矿物学中最广泛使用的矿物质,并提供有关浮石岩石的岩石和地壳分化史的关键信息,从源头到下沉的碎片材料的运输路径'并显着贡献自建议以来的神秘行星级构造事件的重建。然而,对该辅助矿物质的详细纹理分析一直受到二维(2D)分析限制的阻碍。随着X射线纳米分析技术的进步,现在可以非破坏性地,以数字方式,在锆石内,它们的生长和分区模式和三维微量元素的化学分布和量化的内部纹理(3D) )。我们介绍了一种使用同步辐射纳米射游的新型多模式方法,以在〜100〜NM分辨率下进行3D纳米射周的3D纳米氧化锆,证明了通过来自中央芬兰花岗岩复合物的古典古锆吉隆的技术能力。除了晶格参数和锆内的包涵体之外,集成X射线吸收,衍射和荧光断层扫描揭示了3D中的扇区和振荡分区图案以及微量元素之间的分区图案的差异。多峰同步纳米分析纳米图阐明了前所未有的细节中杂交率大小的3D纳米型氧化锆和微量元素组成。

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