The Primary Scope Of This Text-Book Covers The Transmission As Well As Reflection Optics Of Minerals And The Methods Of Their Studies. To Explain The Optical Behaviour Of Minerals, Some Relevant Concepts In Spectroscopy Have Been Introduced. This Book Fills The Need Of The Students To A Better Understanding Of The Physical Nature Of Minerals Through Studies In Ir-Visible-X-Ray Region.This Book Contains Seven Chapters Titled As: General Optics: Interactions Of Light With Matter, Study In Polarised Light, Optical (Absorption) Sepctroscopic Studies Of Minerals, Reflection Optics, Reflection Spectroscopy, Vibrational Spectroscopy: Infrared And Raman - An Outline, X-Ray Optics. It Also Offers As Appendices The Transmission, Reflection Properties And X-Ray Data Of Minerals.This Is The Only Book That Lucidly Introduces The Principles Of Modern Methods Of Mineral Optics In A Single Volume For The Students Of Graduate And Post-Graduate Levels.

International Tables for Crystallography is the definitive resource and reference work for crystallography and structural science. Each of the volumes in the series contains articles and tables of data relevant to crystallographic research and to applications of crystallographic methods in all sciences concerned with the structure and properties of materials. Emphasis is given to symmetry, diffraction methods and techniques of crystal-structure determination, and the physical and chemical properties of crystals. The data are accompanied by discussions of theory, practical explanations and examples, all of which are useful for teaching. Volume C provides the mathematical, physical and chemical information needed for experimental studies in structural crystallography. This volume covers all aspects of experimental techniques, using all three principal radiation types (X-ray, electron and neutron), from the selection and mounting of crystals and production of radiation, through data collection and analysis, to interpretation of results. Each chapter is supported by a substantial collection of references, and the volume ends with a section on precautions against radiation injury. Eleven chapters have been revised, corrected or updated for the third edition of Volume C. More information on the series can be found at: http://it.iucr.org

Structures of layer silicates; order-disorder in clay mineral structures; interlayer and intercalation complexes of clay minerals; interstratified clay minerals; X-ray diffraction procedures for clay mineral identification; associated minerals; quantitative X-ray mineral analysis of clays; appendix: tables for the determination of d in Å from 20 for the Ka and Kb radiations of copper, cobalt and iron.

The decision of Springer-Verlag to publish this book in English came as a pleasant surprise. The fact is that I started writing the first version of the book back in 1978. I wished to attract attention to potentialities inherent in selected-area electron diffraction (SAED) which, for various reasons, were not being put to use. By that time, I had at my disposal certain structural data on natural and synthetic minerals obtained using SAED and high-resolution electron microscopy (HREM), and this stimulated my writing this book. There were several aspects concerning these data that I wished to emphasize. First, it was mostly new and understudied minerals that possess the peculiar structural features studied by SAED and HREM. This could interest mineralogists, crystallo chemists, and crystallographers. Second, the results obtained indi cated that, under certain conditions, SAED could be an effective, and sometimes the only possible, method for structure analysis of minerals. This inference was of primary importance, since fine dispersion and poor crystallinity of numerous natural and synthe tic minerals makes their structure study by conventional diffrac tion methods hardly possible. Third, it was demonstrated that in many cases X-ray powder diffraction analysis of dispersed miner als ought to be combined with SAED and local energy dispersion analysis. This was important, since researchers in structural min eralogy quite often ignored, and still ignore even the simplest in formation which is readily available from geometrical analysis of SAED patterns obtained from microcrystals.