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Titlebook: Electron-Diffraction Analysis of Clay Mineral Structures; Boris Borisovich Zvyagin Book 1967 Springer Science+Business Media New York 1967

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發(fā)表于 2025-3-23 13:40:18 | 只看該作者
https://doi.org/10.1007/978-3-031-41705-4We have already noted that the general expression for the structure amplitude [formulas (4)–(6) in Chapter 3], i.e., for the scattering by the atoms of one cell, is given by an integral taken over the volume of the unit cell:
12#
發(fā)表于 2025-3-23 15:12:30 | 只看該作者
Experimental Electron - Diffraction Methods of Studying Minerals,The basis of the electron-diffraction method was the discovery, in 1927, of the phenomenon of electron diffraction. It was shown that electrons, like any other atomic particles, possess wave properties.
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發(fā)表于 2025-3-23 18:29:02 | 只看該作者
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發(fā)表于 2025-3-23 22:58:39 | 只看該作者
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發(fā)表于 2025-3-24 13:37:00 | 只看該作者
Structures and Structure Modifications of Layer Silicates,centers of the polyhedra are arranged in a hexagonal pattern (Figs. 2–4). The tetrahedral and octahedral networks, which are of similar dimensions, are connected together into layers, and in any given mineral group all the layers are formed from a given combination of these networks.
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發(fā)表于 2025-3-25 02:47:44 | 只看該作者
https://doi.org/10.1007/978-3-540-70974-9centers of the polyhedra are arranged in a hexagonal pattern (Figs. 2–4). The tetrahedral and octahedral networks, which are of similar dimensions, are connected together into layers, and in any given mineral group all the layers are formed from a given combination of these networks.
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