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- W1485192642 abstract "Upper Cretaceous to mid-Tertiary sediments of the inner Coastal Plain sketchily record a long interval of intense weathering, erosion, and deposition in a passive area that was inundated and reexposed, repeatedly, by major fluctuations of sea level. Low to moderate relief was maintained for more than 90 my while the area alternated between inner coastal plain and inner continental shelf. Regressions are marked by fluvial kaolinitic sands and clays and well zoned weathering profiles. Transgressions are marked by littoral sands and by neritic clays and carbonates . Kaolinite-rich detritus transported to the inner Coastal Plain originated through weathering of metamorphic and igneous rocks of the Piedmont Upland. Most of the sediments underwent more than one stage of sorting and weathering. Some were significantly modified by post-depositional leaching, oxidation, and diagenesis. Commercial kaolins are found where successive stages favored both beneficiation and final preservation. Three types of kaolin can be distinguished: soft, hard, and flint. The first two types are commercial. Superb exposures of the sediments and associated kaolins are provided by large opencut kaolin mines in this area, which is one of the world's larger producers of industrial clay." @default.
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- W1485192642 date "2013-03-17" @default.
- W1485192642 modified "2023-09-24" @default.
- W1485192642 title "Cretaceous-Tertiary Strata and Kaolin Deposits in the Inner Coastal Plain of Georgia" @default.
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- W1485192642 doi "https://doi.org/10.1029/ft172p0002" @default.
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