Midale lithofacies and distribution

Productive facies

The Midale in the Weyburn area is carbonates and evaporites deposited near a low-energy shoreline on a marine ramp. The main producing carbonate facies (“vuggy pack-stone” facies) is shoal deposits of fossiliferous, peloidal, Ortonella-bearing nodular wacke-stones to grainstones. The principal occluding cements are sparry calcite and anhydrite.

Reservoir SEM and capillary pressure curve

The figure below shows the petrophysical characteristics of the main Weyburn reservoir facies: Ortonella-bearing vuggy wackestones to packstones. The sample is macroporous, its pore system dominated by large pores and pore throats. The capillary pressure curve shows relatively low entry (and presumably breakthrough) pressure. The port size (r₃₅) of the sample is approximately 3μ.

Figure 9-99 See text for explanation.

Nonproductive facies

The main nonproductive updip carbonate facies (“porous mudstone”) is locally laminated and burrowed peloidal lime and dolomite mudstones to wackestones. These tighter rocks originated on a low-energy to restricted shelf and in lagoons.

Nonreservoir SEM and capillary curve

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 r₃₅ and r₁₀ values for the sample are 0.2 and 0.25μ, respectively.

Figure 9-100 See text for explanation.

Facies tracts of midale vuggy beds

The Midale Vuggy beds contain three facies tracts that parallel the paleo-shoreline (northwest).

In and downdip from Weyburn field, the rocks consist primarily of the vuggy packstone facies, although there are numerous thin interbeds of porous mudstone facies.
Landward (now updip) from this facies tract, the reservoir grades into porous mudstone facies with scattered lenses of poorly developed, vuggy packstone facies.
Still farther northeast but downdip from the truncation edge of the Midale, the rocks change facies into anhydrite.

Overlying and underlying beds

The beds overlying the Midale Vuggy, i.e., the Midale Marly beds, consist almost entirely of the porous mudstone facies. The beds underlying the Midale Vuggy are tight carbonates and evaporites.

Weyburn well log

The figure below is an example of log characteristics of Midale beds in a Weyburn field well. The well was continuously cored through the Midale interval. The brick pattern denotes packstone facies with vuggy and intergranular porosity; hachures indicate porous dolomitic mudstone facies. Log and core data for representative (if extreme) data points, numbered 1-8, also appear in Figures 9-102 through 9-104.

Figure 9-101 From .^[1]

References

↑ Coalson, E., B., Hartmann, D., J., Thomas, J., B., 1990, Applied Petrophysics in Exploration and Exploitation: Notes from short course sponsored by Univ. of Colo.–Denver, var. pages.

External links

find literature about
Midale lithofacies and distribution

[ch09r11-1] Coalson, E., B., Hartmann, D., J., Thomas, J., B., 1990, Applied Petrophysics in Exploration and Exploitation: Notes from short course sponsored by Univ. of Colo.–Denver, var. pages.

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