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Line 43: − The figure below shows (1) a typical succession of carbonate lithofacies sequences that formed during high-amplitude, high-frequency sea level fluctuations and (2) a corresponding sea level curve related to diagenesis. In this example, sequences lack internal barriers or seals to inhibit the vertical and lateral migration of the paleowater table; therefore, sequence sediments are subjected to a complex sequence of diagenetic events due to large-scale sea level fluctuations. If internal barriers were present, diagenesis would be lessened. − + + +
Sequences during high-amplitude, high-frequency cycles (view source)
Revision as of 15:49, 20 February 2014
, 15:49, 20 February 2014→High-amplitude sequences schematic
==High-amplitude sequences schematic==
==High-amplitude sequences schematic==
[[file:predicting-reservoir-system-quality-and-performance_fig9-83.png|thumb|{{figure number|9-83}}.]]
[[file:predicting-reservoir-system-quality-and-performance_fig9-83.png|thumb|{{figure number|1}}.]]
[[:file:predicting-reservoir-system-quality-and-performance_fig9-83.png|Figure 1]] shows (1) a typical succession of carbonate lithofacies sequences that formed during high-amplitude, high-frequency sea level fluctuations and (2) a corresponding sea level curve related to diagenesis. In this example, sequences lack internal barriers or seals to inhibit the vertical and lateral migration of the paleowater table; therefore, sequence sediments are subjected to a complex sequence of diagenetic events due to large-scale sea level fluctuations. If internal barriers were present, diagenesis would be lessened.
==See also==
==See also==