On the Determination of Sediment Accumulation Rates
Published on 14. June 1999
Book
Paperback/Softback
256 pages
978-0-87849-837-6 (ISBN)
Description
Sediment accumulation rates are an essential tool for the understanding of processes related to the deposition of organic and inorganic materials in marine and lacustrine environments. Sediment accumulation rates are not only a measure of the speed of deposition, but also represent a very useful tool for further paleoenvironmental reconstructions of climate history or biotic evolution as seen in the fossil record.
More details
Language
English
Place of publication
Zurich
Switzerland
Target group
Professional and scholarly
Illustrations
Illustrations, unspecified
Dimensions
Height: 24 cm
Width: 17 cm
Thickness: 1.3 cm
Weight
610 gr
ISBN-13
978-0-87849-837-6 (9780878498376)
DOI
10.4028/www.scientific.net/RC.39
Schweitzer Classification
Other editions
Additional editions
Peter Bruns | H.C. Hass | Trans Tech Publications Ltd
On the Determination of Sediment Accumulation Rates
E-Book
06/1999
Trans Tech Publications Ltd
€171.20
Available for download
Peter Bruns | H.C. Hass
On the Determination of Sediment Accumulation Rates
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06/1999
Trans Tech Publications Ltd
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Content
Preface
On Sediment Accumulation Rates and their Determination
The Influence of Hiatuses on Sediment Accumulation Rates
Coccolithophore Export Production and Accumulation Rates
Estimating Marine Sediment Accululation Rates from Geochemical Pore Water Gradients
Sedimentation Rates of Late Quaternary Periplatform Sediments Based on Aragonite/Calcite Ratios: Sudanese Red Sea versus Petro Bank(Caribbean)
Lateral Changes of Mass Accumulation Rates Derived from Seismic Reflection Profiles: An Example from the Western Atlantic
Determination of Mass Accumulation Rates from Cosmic Particle Fluxes
Determining Sedimentation Rates Using Luminescence Dating
New Absolute Dating Techniques for Quaternary Sediments and their Application on the Russian Plain
A Stratigraphic Database for the Atlantic Ocean Sediment Record: SYNATLAN (SYNthesis ATLANtic); Bioevents and Hiatuses in the Meso- and Cenozoic Atlantic, Age-Depth Models, (DSDP/ODP Drillsite Data)
210Pb- and 137Cs-Based Sediment Accumulation Rates in Inner Shelves and Coastal Lakes of Subarctic and Arctic Alaska: A Synthesis
Sedimentation Rates and Late Holocene Climate Change: A Case Study from the Skagerrak (NE North Sea)
Holocene Pelagic and Turbidite Sedimentation Rates in the Amerasia Basin, Arctic Ocean from Radiocarbon Age-Depth Profiles in Cores
Late Quaternary Variations in Sediment Accumulation Rates and their Paleoenvironmental Implications: A Case Study from the East Greenland Continental Margin
On Sediment Accumulation Rates and their Determination
The Influence of Hiatuses on Sediment Accumulation Rates
Coccolithophore Export Production and Accumulation Rates
Estimating Marine Sediment Accululation Rates from Geochemical Pore Water Gradients
Sedimentation Rates of Late Quaternary Periplatform Sediments Based on Aragonite/Calcite Ratios: Sudanese Red Sea versus Petro Bank(Caribbean)
Lateral Changes of Mass Accumulation Rates Derived from Seismic Reflection Profiles: An Example from the Western Atlantic
Determination of Mass Accumulation Rates from Cosmic Particle Fluxes
Determining Sedimentation Rates Using Luminescence Dating
New Absolute Dating Techniques for Quaternary Sediments and their Application on the Russian Plain
A Stratigraphic Database for the Atlantic Ocean Sediment Record: SYNATLAN (SYNthesis ATLANtic); Bioevents and Hiatuses in the Meso- and Cenozoic Atlantic, Age-Depth Models, (DSDP/ODP Drillsite Data)
210Pb- and 137Cs-Based Sediment Accumulation Rates in Inner Shelves and Coastal Lakes of Subarctic and Arctic Alaska: A Synthesis
Sedimentation Rates and Late Holocene Climate Change: A Case Study from the Skagerrak (NE North Sea)
Holocene Pelagic and Turbidite Sedimentation Rates in the Amerasia Basin, Arctic Ocean from Radiocarbon Age-Depth Profiles in Cores
Late Quaternary Variations in Sediment Accumulation Rates and their Paleoenvironmental Implications: A Case Study from the East Greenland Continental Margin