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* [[Porosity]] in the sequence tops plugged by caliche and vadose fibrous cements
 
* [[Porosity]] in the sequence tops plugged by caliche and vadose fibrous cements
 
* [[Porosity]] in subtidal grainy parts of sequences generally lacks early sparry cements; primary porosity preserved where marine fringing cement present
 
* [[Porosity]] in subtidal grainy parts of sequences generally lacks early sparry cements; primary porosity preserved where marine fringing cement present
* Top and lateral seals may form where peritidal dolomite and evaporite progrades over [[third-order sequences]]
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* Top and lateral seals may form where peritidal dolomite and evaporite [[Well_log_sequence_analysis#Parasequence_stacking_patterns|prograde]] over [[third-order sequences]]
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An example is the Late Mississippian ramp reservoirs of the eastern and central United States.
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An example is the Upper Mississippian ramp reservoirs of the eastern and central United States.
    
==Humid zone characteristics==
 
==Humid zone characteristics==
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