The
stratigraphy of fluvial systems in rift basins records the complex interactions
of numerous internal and external forcing mechanisms. To better understand the controls on alluvial architecture
in rift basins, Connell et al. examine the relation between surface
processes and stratigraphic variability using an experimental basin, varying subsidence
and sediment flux and observing stratigraphic packaging and variability. The results reveal the changes in
sediment distribution in a setting with well-constrained external boundary
conditions. The data provide novel
insights into how multiple sediment sources impact the stratigraphic position,
size, and composition of axial-river deposits of rift basins.
Stratigraphic Architecture of An Experimental Basin With Interacting Drainages by Sean D. Connell, Wonsuck
Kim, Gary A. Smith, and Chris Paola
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