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 floo...
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| Format: | eBook |
| Language: | English |
| Published: |
Berlin ; New York :
Springer-Verlag,
[1993]
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| Series: | Lecture notes in earth sciences ;
51. |
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| Online Access: | Connect to the full text of this electronic book |
Table of Contents:
- Part 1. The three component system
- Sediment recipes
- Depositional dilution processes with three components
- Factors influencing the three-component system
- Relative time span assessment
- Part 2. Carbonate-organic carbon distribution in beds and sequences
- Input variation in rhythmically bedded sediment
- Combined input pattern of transgressive-regressive cycles, Upper Cretaceous, U.S. Western Inetrior
- Part 3. Carbonate-organic carbon changes in facies transitions
- Carbonate-clastic systems
- Systems rich and poor in organic carbon.