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October 31, 1975 - Gerald R. Ford Presidential Library and Museum

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The Spraberry Trend oil field is located in Upton, Reagan, Irion,<br />

Martin, Midl<strong>and</strong>, <strong>and</strong> Glasscock Counties of West Texas, within the<br />

Midl<strong>and</strong> Basin.<br />

The producing formations are the Upper <strong>and</strong> Lower Spraberry which are<br />

C1earfork-Wichita equivalent of Permian age. The underlying Dean S<strong>and</strong><br />

is Wo1fcamp, also of Permian age. The Upper Spraberry is generally<br />

around 400 feet thick; the Lower Spraberry ranges from 500 to 600 feet<br />

in thickness; <strong>and</strong> the Dean S<strong>and</strong> is about 120 feet thick. Over most of<br />

the area. about 90 percent of the thickness is s<strong>and</strong>, s·i1t. <strong>and</strong> shale<br />

(mostly shale). The remaining 10 percent or so is limestone <strong>and</strong><br />

dolomite. The oil is indigenous to the formation. The reservoir rock<br />

is extremely low in porosity <strong>and</strong> permeability, <strong>and</strong> is a siltstone.<br />

Production is made possible by fractures which extend through both<br />

the matrix siltstone <strong>and</strong> the shale. Depth to the top of the Upper<br />

Spraberry varies from 6,000 to 8,000 feet.<br />

The oil accumulations in the Spraberry are trapped stratigraphically.<br />

The area is virtually devoid of folded or faulted traps. The structure<br />

is a general monocline dipping from the eastern shelf into the depths<br />

of the Midl<strong>and</strong> Basin. The classic sections grade into limestones <strong>and</strong><br />

dolomites on the rims of the basin. The productive field, as defined<br />

by the Texas Railroad Commission, covers 920,000 acres (about 1,400<br />

square miles). The consultant firm also estimates that an additional<br />

150,000 acres on the fringes of the field may be developed in the<br />

future.<br />

The crude oil at Spraberry Trend was initially undersaturated. However,<br />

because of low permeability, pressure was quickly reduced in the<br />

vicinity of producing wells causing release of gas from solution <strong>and</strong><br />

high producing gas/oil ratios. The primary producing mechanism was a<br />

dissolved gas drive. Bottom water is not active. Oil drains from the<br />

siltstone matrix into the fracture system <strong>and</strong> productivity depends on<br />

the effectivel1ess of this fracture system. The normal spacing is 160<br />

acres per well <strong>and</strong> over 3,900 wells are currently producing. About .<br />

320,000 acres or 35 percent of the presently defined area of the field<br />

have been under water flood.<br />

Ultimate recovery by primary methods was determined by preparing<br />

production decline curves for each lease. Primary ultimate recovery<br />

is expected to average 500 barrels per acre. Secondary ultimate<br />

recovery was similarly estimated by studying the production records<br />

for the 34 water flood units. The contractor estimated that additional<br />

secondary recovery will average 200 barrels per acre. These volumes<br />

are considered proved. The secondary recovery reserves for 375,000<br />

acres of future projects are reported under "Indicated Secondary<br />

Reserves." The availability of production decline information <strong>and</strong><br />

the 80 percent extent of depletion of the proved volumes should cause<br />

the reserves estimate to be quite firm.<br />

152

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