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Line 20: − The diagram below shows the sequence of diagenetic events occurring in a prograding tidal flat during a high-frequency sea level cycle. Also shown are two pre-existing topographic highs that were propagated upward through the section by differential compaction. The stippled pattern represents limestone; the brick pattern is dolomite. − + + +
Sea level cycles and carbonate diagenesis (view source)
Revision as of 21:12, 19 February 2014
, 21:12, 19 February 2014→Example
==Example==
==Example==
[[file:predicting-reservoir-system-quality-and-performance_fig9-79.png|thumb|{{figure number|9-79}}Modified. Copyright: Read, 1995; courtesy SEPM.]]
[[file:predicting-reservoir-system-quality-and-performance_fig9-79.png|thumb|{{figure number|1}}Modified. Copyright: Read, 1995; courtesy SEPM.]]
The diagram in [[:file:predicting-reservoir-system-quality-and-performance_fig9-79.png|Figure 1]] shows the sequence of diagenetic events occurring in a prograding tidal flat during a high-frequency sea level cycle. Also shown are two pre-existing topographic highs that were propagated upward through the section by differential compaction. The stippled pattern represents limestone; the brick pattern is dolomite.
The following diagenetic processes occurred during this period.
The following diagenetic processes occurred during this period.