Mapping sedimentary facies and fluvial-aeolian interaction by remote sensing (Sossusvlei, Namib Desert)

Sedimentary facies exert a primary control on sandstone diagenesis and reservoir quality. The Namib Sand Sea with its Sossusvlei playa-lake is often considered as a modern analogue for sandstone reservoirs. Remote sensing in combination with ground observations allowed us to map the facies distribution pattern of associated fluvial and aeolian sediments. Laboratory spectral signature measurements were used to further improve the separability of six major facies: modern aeolian sand, bypass surface, mud pool/mud drapes, heavy mineral lag, aeolian reworked and fossil dune remnant. Using a supervised classification algorithm trained by field observations, a combination of Principal Component Analysis, band ratios, texture and geomorphologic indices has shown the best result. This made it possible to create a map outlining the facies distribution pattern of the Sossusvlei area at a scale of 1:10 000. We propose this as a possible workflow to efficiently map and monitor desert environments and to investigate the interplay of aeolian and fluvial sediments, including their linked implications on diagenesis. This could improve paleoclimate modelling and even allow facies mapping on other planets.