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[[file:exploring-for-stratigraphic-traps_fig21-31.png|left|thumb|{{figure number|1}}See text for explanation.]]
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[[file:exploring-for-stratigraphic-traps_fig21-31.png|300px|left|thumb|{{figure number|1}}See text for explanation.]]
    
==Example: calibrating logs to cores and shows==
 
==Example: calibrating logs to cores and shows==
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[[file:exploring-for-stratigraphic-traps_fig21-32.png|thumb|{{figure number|2}}. Copyright: Putnam and Oliver, 1980; courtesy Canadian Society of Petroleum Geologists. Map courtesy Eric Dahlberg.]]
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[[file:exploring-for-stratigraphic-traps_fig21-32.png|300px|thumb|{{figure number|2}}. Copyright: Putnam and Oliver, 1980; courtesy Canadian Society of Petroleum Geologists. Map courtesy Eric Dahlberg.]]
    
Posting core [[porosity]], permeability, and pore throat radius (r<sub>35</sub>) data directly on wireline logs next to lithofacies descriptions and show data helps us decide about exploitation for stratigraphic traps. In [[:file:exploring-for-stratigraphic-traps_fig21-31.png|Figure 1]], the live oil stain in macroporous strata indicates the direction to move updip. The only macroporous strata present is within an algal mound facies developed in this parasequences at relative highstand. Microporous dolomites comprising the lower portions of the parasequences have poor reservoir characteristics, despite high porosity readings on the logs. Thus, the target of interest is the highstand mound facies.
 
Posting core [[porosity]], permeability, and pore throat radius (r<sub>35</sub>) data directly on wireline logs next to lithofacies descriptions and show data helps us decide about exploitation for stratigraphic traps. In [[:file:exploring-for-stratigraphic-traps_fig21-31.png|Figure 1]], the live oil stain in macroporous strata indicates the direction to move updip. The only macroporous strata present is within an algal mound facies developed in this parasequences at relative highstand. Microporous dolomites comprising the lower portions of the parasequences have poor reservoir characteristics, despite high porosity readings on the logs. Thus, the target of interest is the highstand mound facies.

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