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Line 28: − The figure below illustrates the petrophysical characteristics of the main nonreservoir facies in the field: lime and dolomite mudstones to wackestones. The sample pore system consists of fine intergranular and unconnected vuggy pores and pore throats. The capillary pressure curve shows the higher entry pressure of the nonreservoir facies compared to the reservoir facies. The r<sub>35</sub> and r<sub>10</sub> values for the sample are 0.2 and 0.25μ, respectively. − + + +
Midale lithofacies and distribution (view source)
Revision as of 21:38, 12 February 2014
, 21:38, 12 February 2014→Nonreservoir SEM and capillary curve
==Nonreservoir SEM and capillary curve==
==Nonreservoir SEM and capillary curve==
[[file:predicting-reservoir-system-quality-and-performance_fig9-100.png|thumb|{{figure number|9-100}}See text for explanation.]]
[[file:predicting-reservoir-system-quality-and-performance_fig9-100.png|thumb|{{figure number|2}}See text for explanation.]]
[[:file:predicting-reservoir-system-quality-and-performance_fig9-100.png|Figure 2]] illustrates the petrophysical characteristics of the main nonreservoir facies in the field: lime and dolomite mudstones to wackestones. The sample pore system consists of fine intergranular and unconnected vuggy pores and pore throats. The capillary pressure curve shows the higher entry pressure of the nonreservoir facies compared to the reservoir facies. The r<sub>35</sub> and r<sub>10</sub> values for the sample are 0.2 and 0.25μ, respectively.
==Facies tracts of midale vuggy beds==
==Facies tracts of midale vuggy beds==