Silicon is a metalloid having the diamond structure (Fig. 1). It has the appearance of a metal (Fig. 2) but lacks all properties of metals. Modern electronics is almost exclusively (>95%) based on silicon devices and these are made from single-crystal silicon. Silica, SiO2, is the major constituent of rock-forming minerals in magmatic and metamorphic rocks; it accounts for ca. 75% of the Earth’s crust. The basic building block of the silicates is the SiO 4−4 tetrahedron (Fig. 3). The variety in the structures of the silicates is due to the various possible combinations of these tetrahedral, both with each other and also with other ions.
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References
Habashi F (2003) Metals from ores. An introduction to extractive metallurgy. Métallurgie Extractive Québec, Québec City. Distributed from Laval University Bookstore. www.zone.ul.ca
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Habashi, F. (2013). Silicon, Physical and Chemical Properties. In: Kretsinger, R.H., Uversky, V.N., Permyakov, E.A. (eds) Encyclopedia of Metalloproteins. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-1533-6_405
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DOI: https://doi.org/10.1007/978-1-4614-1533-6_405
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