Overview: Sedimentation as a Three-Component System describes the mostcommon stylesof deposition in marine environments as theyrelate to sediment composition.Three components, organicmatter, carbonate, and siliciclastic sediment, maysettleconcurrently, but at different rates, intermixing on the seafloor to form a particular sediment composition. A change intheflux of one component is capable of relatively dilutingor concentrating theother two components, which can beexpressed in the characteristic ratio of organic carbon tocarbonate in the resulting sediment. The basic conceptofthis book is to
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