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- W141124902 abstract "Diatomites are formed in both marine and freshwater systems where the processes of diatom formation, diatom preservation, and sedimentation conspire to produce diatomaceous sediments. Diatomite formation seems to have been particularly prevalent in the Miocene, the Plio-Pleistocene, and during the early to middle Holocene periods. Because of the properties conferred on diatomite sediment by a high silica content and a fine-grained texture, these extensive natural deposits are often exploited commercially. Such deposits are either marine or freshwater in origin and terrestrial exposures are mined in both the northern and southern hemispheres. Commercial extraction of diatomites began less than 200 years ago, but diatomites have been exploited for building products since at least the first millennium BC. Diatomites have a variety of modern uses and recently they are proving to be a useful additive for improving the quality of cements and other building products. They have been undervalued as proxies for past environmental change and for indicating evolutionary trends in diatoms." @default.
- W141124902 created "2016-06-24" @default.
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- W141124902 date "2013-01-01" @default.
- W141124902 modified "2023-09-29" @default.
- W141124902 title "DIATOM METHODS | Diatomites: Their Formation, Distribution, and Uses" @default.
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- W141124902 doi "https://doi.org/10.1016/b978-0-444-53643-3.00220-x" @default.
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