In deltaic deposits, the largest volumes of sandy deposits occur at the delta top (as channel accretion, overbank deposits) and as distinct or amalgamated sandy mouth bars in the upper delta front. We use process-based models to study the sediment distribution in four evolving deltas, each with a different input sediment profile. We show how the mouthbar deposits can preserve a large proportion of the sand preserved in the sedimentary record of deltaic systems.
|Number of pages||1|
|Publication status||Published - 2018|
|Event|| International Meeting of Sedimentology 2017: 33rd IAS & 16th ASF Joint Meeting - Toulouse, France|
Duration: 10 Oct 2017 → 12 Oct 2017
|Conference||International Meeting of Sedimentology 2017|
|Period||10/10/17 → 12/10/17|