Spatial Distribution and Connectivity of thin-bedded crevasse splay sandstones; outcrop-analogue studies for tough gas reservoir potential

A majority of the volume of alluvial sequences consists of fine-grained floodplain deposits (Kraus, 1987; Kraus & Gwinn, 1997). Traditionally, these deposits are seen as non-reservoir rock since their permeability is very low. This research shows that crevasse splay deposits that occur in these floodplain fines can comprise stacked complexes of...