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all geography including DSDP/ODP Sites and Legs
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Primary terms
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Asia
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GeoRef Categories
Date
Availability
Wenjiite, Ti 10 (Si,P,☐) 7 , and kangjinlaite, Ti 11 (Si,P) 10 , new minerals in the ternary Ti-P-Si system from the Luobusa ophiolite, Tibet, China Available to Purchase
Wodegongjieite, ideally KCa 3 (Al 7 Si 9 )O 32 , a new sheet silicate isostructural with the feldspar polymorph kokchetavite, KAlSi 3 O 8 Open Access
3D electron diffraction study of terrestrial iron oxide alteration in the Mineo pallasite Available to Purchase
Jingsuiite, TiB 2 , a new mineral from the Cr-11 podiform chromitite orebody, Luobusa ophiolite, Tibet, China: Implications for recycling of boron Available to Purchase
The Effect of the Starting Mineralogical Mixture on the Nature of Fe-Serpentines Obtained during Hydrothermal Synthesis AT 90°C Available to Purchase
Dolomite-IV: Candidate structure for a carbonate in the Earth's lower mantle Available to Purchase
Electron crystallography Available to Purchase
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.