The geomorphology, stratal
architecture, and sedimentologic attributes of a range of deltas have been
interpreted in the context of fluvial, tidal, and wave processes and sea-level
change. Most studies focus on delta-front regions, whereas finer (and typically
less well exposed) delta plain deposits have received less attention. Here,
Gugliotta et al. focus on defining and describing tide-influenced crevasse
subdelta deposits, an important component of lower delta plain stratigraphy of a
river-dominated delta in the Lajas Formation of the Neuquén Basin of Argentina.
The study emphasizes the importance of understanding the relative importance of
tide and river processes in facies distribution and architecture, and the
applications to characterization of interdistributary deposits. The data suggest
that some “tidal” deposits interpreted from the rock record may instead be
river-dominated, tide-influenced crevasse subdeltas, and that this distinction
has important implications for understanding paleogeography and predicting
reservoir geometries.
Stratigraphic record of river-dominated crevasse subdeltas with tidal influence (Lajas Formation, Argentina) by Marcello Gugliotta, Stephen S. Flint, David M. Hodgson, and
Gonzalo D. Veiga
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