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Download e-book for iPad: An Introduction to Mineral Sciences by Andrew Putnis

By Andrew Putnis

ISBN-10: 0521429471

ISBN-13: 9780521429474

The topic of mineralogy has moved clear of the systematic remedy of mineral teams towards the learn of the habit of minerals in line with geological approaches. it is crucial that we comprehend the physics and chemistry of minerals as this reaction commonly comprises structural and chemical adjustments inside of person minerals in addition to reactions among minerals. this is often the 1st textual content to supply an advent to trendy mineralogy for undergraduate scholars. the most, and infrequently complicated, innovations required to appreciate minerals and the techniques that happen inside of them are offered in a simple to keep on with demeanour with none advanced mathematical therapy. The booklet bargains with solid-state ameliorations in minerals, which happen according to alterations in temperature and strain, in addition to introducing the fundamental crystallography, physics and chemistry had to comprehend those procedures. No wisdom of physics, chemistry and arithmetic past high-school point is believed.

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Extra resources for An Introduction to Mineral Sciences

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G. in the tetragonal system the direction [Oil] is no longer at 45° to [010], nor is it the same direction as the normal to the plane (Oil). chemistry. Holt, Reinhart & Winston Inc. J. (1970). Contemporary crystallography. McGraw-Hill Book Co. S. (1977). Crystallography and its applications. Van Nostrand Reinhold. KELLY, A. W. (1970). Crystallography and crystal defects. Longman. McKlE, D. AND McKlE, C. (1986). Essentials of crystallography. Blackwell Scientific Publications. STEADMAN, R. (1982).

Note however that in point group 222 this would be reduced to 4. As well as being able to describe the orientation of planes and directions in a crystal, we also often need to deal with the relationship between planes and directions, and of most importance is the concept of a zone and a zone axis. A set of planes lie in the same zone if they are all parallel to a common direction [UVW]. The direction [UVW] is called the zone axis. We can visualize this easily in relation to the six faces of a cube.

Examples showing lattice directions in a twodimensional lattice. Note that in general, a lattice direction is not parallel to the normal to a plane indexed with the same integers. This is illustrated by the relationship between the plane (110), shown as a dashed line, and the direction [110]. (hkl) is parallel to the direction [UVW] is given by the Weiss zone law: h\] + k\ + AV = 0 If two planes (hkl) and (h'k'V) lie in the same zone [UVW] then both the above equation and h'U + k'V + /'W = 0 must be satisfied.

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An Introduction to Mineral Sciences by Andrew Putnis

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