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transmission electron microscopy
The glass transition temperature of anhydrous amorphous calcium carbonate
Analytical Techniques for Identification and Characterization of Extraterrestrial Organic Matter
Germanium-rich nanoparticles in Cu-poor sphalerite: A new mechanism for Ge enrichment
Analyses under the curve, identifying how invisible gold is held in pyrite
Atomic-scale structure and non-stoichiometry of meteoritic hibonite: A transmission electron microscope study
Trace-element remobilisation from W–Sn–U–Pb zoned hematite: Nanoscale insights into a mineral geochronometer behaviour during interaction with fluids
Identification of interstratified mica and pyrophyllite monolayers within chlorite using advanced scanning/transmission electron microscopy
Bizarre artefacts in transmission electron microscopy preparation and observation of geological samples
Application of scanning electron diffraction in the transmission electron microscope for the characterisation of dislocations in minerals
Electron channeling to achieve the full potential of mineralogy
Analysis of the structures of minerals is an important part of mineralogical investigations. Mineral assemblies are often formed by micro- or even nanocrystals, and it is most interesting to be able to shed light on the crystallography of individual grains, their structure, crystallinity and other properties. This can be done efficiently by the techniques of transmission electron microscopy. Transmission electron microscopy offers not only an ultimate spatial resolution in the imaging mode, but also the possibility of performing diffraction experiments and structure analysis of very small crystals, as well as a range of spectroscopic techniques revealing chemical composition and other properties of the crystals. This chapter reviews the basic techniques of transimssion electron microscopy and their application in mineralogical crystallography. A special emphasis is put on the methods of structure analysis of nanocrystals. This field has seen a rapid evolution in recent years, and has transformed from a being niche technique to a widely accepted and commonly used method of structure analysis. Its applications in mineralogy are especially rich and attractive.