Zusammenfassung
Die dominierende Rolle der natürlichen Silikate (einschließlich Quarz) besteht darin, dass sie mit einem Anteil von etwas über 90 Vol.-% am stofflichen Aufbau der Erdkruste beteiligt sind (Tabelle 1.5, S. 29). Darüber hinaus besitzen sie eine überragende technische und wirtschaftliche Bedeutung als mineralische Rohstoffe.
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Okrusch, M., Matthes †, S. (2010). Silikate. In: Mineralogie. Springer-Lehrbuch. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-78201-8_9
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