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...[[river-mouth bar]]s, [[interdistributary bay]]s, [[tidal flat]]s, [[tidal ridge]]s, [[beaches]], [[Lithofacies_and_environmental_analysis_of_clastic_deposi ...tidal influence; thus a lower delta plain is most extensive in areas where tidal ranges are large and seaward gradients and topographic relief are low. The

| ''Tidal-zone carbonates'' || colspan = 5 | ''Tidal channel'' ...'' || rowspan = 3 | ''Marine carbonate pinch-outs'' || ''Tidal zone'' || ''Tidal-flat carbonate pinch-out'' || colspan = 4 | ''Pinch-out into silts and shal

| Common tidal and fluvial channel fills || || Permeability contrast with shore face or b | Lagoonal sandstone bodies (washover fans and flood-tidal deltas) can be wholly or partially enclosed in [[mudstone]] || || Can form

| Tidal-dominated delta || - || Low recoveries caused by complex geometry and numer ...orized into three classes in terms of sedimentary process: wave dominated, tidal dominated, and fluvial dominated ([[:file:M91FG185.JPG|Figure 2]]).<ref nam

...issuing ambient water, bottom slope seaward of the mouth, tidal range and tidal currents within the lower river channel, and the ability of waves and other In the absence of high tidal range and extremely strong marine energy, the [[distributary channel]] patt