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- W2028683628 abstract "Abstract Coastal deposits are very dynamic systems that may not have constant sediment accumulation rates over time. High-resolution reconstruction and dating of coastal environments, e.g. timing of vertical accretion of dune and/or beach ridges, can be achieved when collection of samples is closely-spaced, although this method is not always economically viable or time-effective. The low terrestrial dose rate environment leads to an unusual situation in which sample ages depend on the rate of accumulation of the overburden. By mathematically coupling successive sample ages obtained from vertical sediment cores, we are able to provide constraints on the model accumulation profiles. The dependence of sample age on the accumulation model is presented, and sample ages are compared with leading accumulation models of dune and beach ridge formation." @default.
- W2028683628 created "2016-06-24" @default.
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- W2028683628 date "2012-07-01" @default.
- W2028683628 modified "2023-09-27" @default.
- W2028683628 title "OSL and sediment accumulation rate models: Understanding the history of sediment deposition" @default.
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- W2028683628 doi "https://doi.org/10.1016/j.quageo.2012.02.026" @default.
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