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1995 | OriginalPaper | Buchkapitel

Erosion, Sedimentation and Sedimentary Origin of Clays

verfasst von : S. Hillier

Erschienen in: Origin and Mineralogy of Clays

Verlag: Springer Berlin Heidelberg

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Of all the various types of sediment, fine-grained sediments with a high proportion of clay minerals are by far the most abundant. In the marine environment, terrigenous (land-derived) muds cover about 60% of the continental shelves, and almost 40% of the deep ocean basins, amounting in total to about a third of the Earth’s surface (Fig. 4.1). Similarly, although proportionally much smaller in area, continental aquatic environments are often dominated by fine-grained sediments, and these environments include many of the rivers, lakes, deltas and estuaries used extensively by man.

Metadaten
Titel
Erosion, Sedimentation and Sedimentary Origin of Clays
verfasst von
S. Hillier
Copyright-Jahr
1995
Verlag
Springer Berlin Heidelberg
DOI
https://doi.org/10.1007/978-3-662-12648-6_4