Abstract
The Earth is composed of rocks. Rocks are aggregates of minerals. Minerals are composed of atoms. In order to understand rocks, we must first have an understanding of minerals. In order to understand minerals we must have some basic understanding of atoms—what they are and how they interact with one another to form minerals. A particular mineral cannot be formed unless the chemical ingredients necessary to make the mineral are present. Thus, the most common minerals are those that have a chemical composition made of the common elements found in their environment. The atomic bonds of minerals, rules governing the chemistry of the minerals, the different modes of their formation, inter-relationship between mineral species form the basis of mineral chemistry and shall be discussed in this chapter.
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Further Reading
Blackburn, W.H. and W.H. Dennen. Principles of Mineralogy, 2nd ed. William C. Brown, Dubuque, IA. 1994.
Bloss, F. Donald. Crystallography and Crystal Chemistry. Holt Rinehart, Winston, New York. 1971.
Deer, W.A., R.A. Howie and J. Zussman. Rock Forming Minerals. 5 vols. John Wiley and Sons, New York. 1962.
Henderson, Paul. Inorganic Geochemistry. Pergamon, New York. 1982.
Klein, C. and C.S. Hurlbut, Jr. Manual of Mineralogy, 21st ed. John Wiley and Sons, New York. 1993.
Pauling, Linus. The Nature of the Chemical Bond, 3rd Edition. Cornell Univ. Press, Ithaca, NY. 1960.
Smyth, J.R. and D.L. Bish. Crystal Structures and Cation Sites of the Rock Forming Minerals. Allen and Unwin, London. 1988.
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Mukherjee, S. (2011). Mineral Chemistry. In: Applied Mineralogy. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-1162-4_3
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DOI: https://doi.org/10.1007/978-94-007-1162-4_3
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-007-1161-7
Online ISBN: 978-94-007-1162-4
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