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- W1526111184 abstract "The mineralogy of chert recovered in the central Pacific at several Deep Sea Drilling sites appears strongly influenced by the lithology of host sediments. Chert in clayey sediments is porcelanitic, while quartzose chert nodules are found exclusively in calcareous oozes and rocks. This composition is related to the amount of clay minerals in the sediment. Poor permeability and abundant foreign cations in clay-rich layers lead to precipitation of disordered cristobalite while good circulation and lack of exchangeable cations in carbonates favour direct precipitation of quartz. Chert formation results from a transfer from the highly soluble amorphous silica of biogenic origin into much less soluble crystalline forms. This transfer may be controlled by silico-aluminates present in the sediments. In most of the post-Lower Tertiary sediments these minerals might have been able to take up enough silica from interstitial waters to prevent chert formation." @default.
- W1526111184 created "2016-06-24" @default.
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- W1526111184 date "1975-01-01" @default.
- W1526111184 modified "2023-09-25" @default.
- W1526111184 title "Formation of Deep‐Sea Chert: Role of the Sedimentary Environment" @default.
- W1526111184 doi "https://doi.org/10.1002/9781444304855.ch15" @default.
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