Reservoir quality in fluvial siliciclastic rocks is variable. Permeability is influenced by
micron-scale grain coatings or bedding style on the m- km-scale. Outcrops allow the analysis of
depositional environments and diagenesis thus an investigation of reservoir quality controls.
A process-oriented approach is used to understand variability in a meander deposit compaction
and cementation behavior of lithofacies types during burial and the discrepancy between
porosity and permeability values.
