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...limited [[lateral]] extent and forms in response to (for example) [[tidal flat]] migration or [[Deltaic environments|delta]] lobe shifts. Episodic paraseq ...er|2}}Characteristics of two upward-fining parasequences formed in a tidal flat to subtidal environment. From Van Wagoner et al.;<ref name=ch21r47 /> court

...re number|1}}Sequence of diagenetic events occurring in a prograding tidal flat during a high-frequency sea level cycle. Modified from Read.<ref name=ch09r ...a [[Depocenter#Sediment_supply_rate_and_facies_patterns|prograding]] tidal flat during a high-frequency sea level cycle. Also shown are two pre-existing to

...s,_and_flow_characterization#Carbonate_sediments_and_environments|reefs or tidal flats]]. As a consequence, the primary trap classification of these reservo

...l]]s, [[river-mouth bar]]s, [[interdistributary bay]]s, [[tidal flat]]s, [[tidal ridge]]s, [[beaches]], [[Lithofacies_and_environmental_analysis_of_clastic_ ...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 shales''

...[[Well_log_sequence_analysis#Parasequence_stacking_patterns|aggraded]] and flat topped to gently sloping * Peritidal parasequences with regionally extensive tidal flat caps

* Flat-topped platforms with layer cake, 1–10-m-thick fourth-order sequences bou * Tidal flat facies absent except adjacent to shorelines

Sheet sands are flat to gently undulating bodies of sand that commonly surround dune fields.<ref ...iment are delta, beach, and barrier island, estuarine, lagoonal, and tidal flat.

...ional environments. From shore to basin, they are ''[[peritidal]]'' (tidal flat), ''[[shallow shelf interior]], [[shelf margin complex]], [[slope]]'', and ...idal current]]s are concentrated in channels between islands and produce [[tidal delta]]s on the lee side of the island.

* Rare tidal-flat facies

| 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

...used for establishing sandstone body geometry should have a depositionally flat datum (such as a [[bentonite]] bed, marine shale bed, or laterally persiste ** Tidal flats

...er regressive hemicycle. The transgressive hemicycle is dominated by tidal flat sediments (laminated mudstone and wackestone) and subtidal deposits (e.g., ..., v. 91, no. 1, p. 69–96.</ref> where geometric data for ooid shoal, tidal flat, and eolian carbonate macroforms were used for constructing a 3-D reservoir

|   Tidal flat and estuary |   Back barrier apron and tidal delta

| Tidal-dominated delta || Papua and New Guinea || 8&deg;34'51.89"S || 143&deg;25'2 | Clastic tidal flat || Netherlands || 53&deg;11'31.51N || 4&deg;59'52.95"E

| 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

...tary [[evaporite]] or barren [[salt flat]]s, where intricate networks of [[tidal creek]]s occur and are separated by broad evaporative sequences. From the s ...e often, however, they partially open to the sea or connect to it by small tidal channels. Most of the bays are shallow-water bodies, rarely exceeding 7 to

...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

...facies architecture reveals a more dynamic interaction of river, wave, and tidal processes than is indicated by external shape: Journal of Sedimentary Resea ...ase bounding surface was flattened, to mimic clinoform progradation over a flat, horizontal sea floor, and isochore maps were used to modify the geometries

...ed extra elements favorable for the development of an unconventional play: flat geomorphology, low population density, easy water access, limited competiti ...file:M125-VacaMuerta-Figure5.jpeg|Figure 5]]). Right: line drawing showing tidal oolitic grainstone shoals and carbonate buildups in the topset; bottom-curr