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→Upward-shoaling cementation and compaction reservoir model
===Upward-shoaling cementation and compaction reservoir model===
===Upward-shoaling cementation and compaction reservoir model===
[[file:carbonate-reservoir-models-facies-diagenesis-and-flow-characterization_fig3.png|thumb|{{figure number|3}}Schematic diagrams of the upward-shoaling cementation and compaction reservoir model and the subtidat-supratidal dolomitlzation and sulfate emplacement reservoir model.]]
[[file:carbonate-reservoir-models-facies-diagenesis-and-flow-characterization_fig3.png|300px|thumb|{{figure number|3}}Schematic diagrams of the upward-shoaling cementation and compaction reservoir model and the subtidat-supratidal dolomitlzation and sulfate emplacement reservoir model.]]
The upward-shoaling model is based on a depositional model of sediment [[Aggradation|aggrading]] to sea level. As the water shallows, the energy conditions increase, resulting in a vertically stacked sequence from [[mudstone]]s and [[wackestone]]s at the bottom to [[packstone]]s and [[grainstone]]s at the top ([[:file:carbonate-reservoir-models-facies-diagenesis-and-flow-characterization_fig3.png|Figure 3]]).
The upward-shoaling model is based on a depositional model of sediment [[Aggradation|aggrading]] to sea level. As the water shallows, the energy conditions increase, resulting in a vertically stacked sequence from [[mudstone]]s and [[wackestone]]s at the bottom to [[packstone]]s and [[grainstone]]s at the top ([[:file:carbonate-reservoir-models-facies-diagenesis-and-flow-characterization_fig3.png|Figure 3]]).