There are three major types of sand: terrigenous, carbonate, and pyroclastic. Terrigenous sands are most abundant and are all ultimately derived from outside the basin of deposition by erosion of preexisting crystalline, volcanic, and sedimentary rocks and, except...
CITATION STYLE
Pettijohn, F. J., Potter, P. E., & Siever, R. (1987). Petrography of Common Sands and Sandstones. In Sand and Sandstone (pp. 139–213). Springer New York. https://doi.org/10.1007/978-1-4612-1066-5_5
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