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Line 49: − The diagram below compares moderate-amplitude carbonate sequences from arid zones with carbonate sequences from humid zones. Arid zone grainstones tend to be oolitic, while humid zone grainstones tend to be skeletal. Humid zone sequences show the effects of repeated sea level changes by their distinctive cement zones precipitated in thick meteoric water lenses. − + + +
Sequences during moderate-amplitude, high-frequency cycles (view source)
Revision as of 15:51, 20 February 2014
, 15:51, 20 February 2014→Arid vs. humid zone sequences
==Arid vs. humid zone sequences==
==Arid vs. humid zone sequences==
[[file:predicting-reservoir-system-quality-and-performance_fig9-82.png|thumb|{{figure number|9-82}}Modified. Copyright: Read, 1995; courtesy SEPM.]]
[[file:predicting-reservoir-system-quality-and-performance_fig9-82.png|thumb|{{figure number|1}}Modified. Copyright: Read, 1995; courtesy SEPM.]]
The diagram in [[:file:predicting-reservoir-system-quality-and-performance_fig9-82.png|Figure 1]] compares moderate-amplitude carbonate sequences from arid zones with carbonate sequences from humid zones. Arid zone grainstones tend to be oolitic, while humid zone grainstones tend to be skeletal. Humid zone sequences show the effects of repeated sea level changes by their distinctive cement zones precipitated in thick meteoric water lenses.
==See also==
==See also==