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Titlebook: Electron Microscopy in Mineralogy; H.-R. Wenk Book 1976 Springer-Verlag Berlin · Heidelberg 1976 Elektronenmikroskopie.Mineralogie.crystal

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Contrast Effects at Planar InterfacesMinerals are often known to be to a certain extent disordered structurally as can be deduced from the X-ray diffraction data and occasionally from high-resolution optical microscopy.
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https://doi.org/10.1007/978-3-642-91749-3 system, and focus on the precipitate morphology and on additional analysis of the array of misfit dislocations. It is emphasized that our conclusions on the nature of the misfit dislocations differ significantly from those of Cullen . (1973).
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Introduction light. From . data we can derive accurately the position of atoms in the unit cell on the scale between 1 and 100Å. However such a crystal structure determination gives us an average over many thousands of unit cells, and assumes that all cells are identical.
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On the Detailed Structure of Ledges in an Augite-enstatite Interfaceinopyroxene phase, and the third is the equilibrium phase augite (Champness and Lorimer, 1973, 1974; Lorimer and Champness, 1973; Kohlstedt and Vander Sande, 1973). Discussions of and references to the optical and X-ray data concerning the lamellar precipitates in orthopyroxenes can be found in the papers by Champness and Lorimer.
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