Sedimentation as a three-component system : organic carbon, carbonate, noncarbonate

Sedimentation as a Three-Component System describes the most common styles of deposition in marine environments as they relate to sediment composition.Three components, organic matter, carbonate, and siliciclastic sediment, maysettle concurrently, but at different rates, intermixing on the sea floor...

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Dettagli Bibliografici
Autore principale: Ricken, Werner
Natura: Livre numérique
Lingua:Anglais
Pubblicazione: Berlin ; Paris [etc.] : Springer-Verlag : Springer e-books [20..].
Cham : Springer Nature
Serie:Lecture notes in Earth sciences 51
Soggetti:
Accesso online:Accès sur la plateforme de l'éditeur
Accès sur la plateforme Istex
Accès Université d'Orléans
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Nota: Archives Springer e-books (Licence nationale)
Archives Springer e-books (Licence nationale)
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Edition sous un autre format:• Sedimentation as a three-component system, organic carbon, carbonate, noncarbonate, Werner Ricken, 1993, Berlin, Springer-Verlag, 1 vol. (xii-211 p.), Lecture notes in earth sciences, 978-3-540-57386-9
• Sedimentation as a Three-Component System, Texte imprimé, 9783662201824
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505 0 |a Sediment recipes -- Depositional dilution processes with three components -- Factors influencing the three-component system -- Relative time span assessment -- Input variation in rhythmically bedded sediment -- Combined input pattern of transgressive-regressive cycles, Upper Cretaceous, U.S. Western Interior -- Carbonate-clastic systems -- Systems rich and poor in organic carbon. 
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520 |a Sedimentation as a Three-Component System describes the most common styles of deposition in marine environments as they relate to sediment composition.Three components, organic matter, carbonate, and siliciclastic sediment, maysettle concurrently, but at different rates, intermixing on the sea floor to form a particular sediment composition. A change in the flux of one component is capable of relatively diluting or concentrating theother two components, which can be expressed in the characteristic ratio of organic carbon to carbonate in the resulting sediment. The basic concept of this book is to address organic carbon-carbonate associations in terms of depositional inputs and time spans. In addition, the three-component system describes organic carbon changes related to major facies transitions. Examples include models of the genesis of carbonaceous sediments, with their various laminated to bioturbated lithotypes, and numerical organic carbon prediction. 
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