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(GP/GT) for Additional Water Supply in the Lower Rio Grande

(GP/GT) for Additional Water Supply in the Lower Rio Grande

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The possibility exists <strong>for</strong> this lower section to be cut by<br />

fault<strong>in</strong>g, but <strong>the</strong> sand is persistent and laterally cont<strong>in</strong>uous<br />

throughout <strong>the</strong> area of key well control.<br />

Reservoir Area B<br />

Reservoir Area B is bounded on <strong>the</strong> west by <strong>the</strong> Donna fault<br />

which extends from <strong>the</strong> <strong>Rio</strong> <strong>Grande</strong> northward <strong>in</strong>to Willacy county.<br />

It is bounded on <strong>the</strong> east by <strong>the</strong> Weslaco fault which extends from<br />

<strong>the</strong> <strong>Rio</strong> <strong>Grande</strong> northward along <strong>the</strong> Cameron County-Hidalgo County<br />

l<strong>in</strong>e <strong>in</strong>to Willacy County (Fig. 1). with<strong>in</strong> area B, <strong>the</strong> reservoir is<br />

bounded on <strong>the</strong> south and north by l<strong>in</strong>es which def<strong>in</strong>e <strong>the</strong> limits of<br />

key well control (Fig. 2).<br />

Small faults associated with both <strong>the</strong><br />

Donna and Weslaco faults limit <strong>the</strong> reservoir to <strong>the</strong> north.<br />

The<br />

reservoir may extend somewhat far<strong>the</strong>r to <strong>the</strong> south, but <strong>the</strong> extent<br />

is limited based on available well control. The south edge of <strong>the</strong><br />

reservoir is not affected by <strong>the</strong> Shepherd fault which limits <strong>the</strong><br />

south edge of reservoir area C.<br />

with<strong>in</strong> <strong>the</strong> area outl<strong>in</strong>ed, <strong>the</strong><br />

reservoir could conta<strong>in</strong> as much as 120 square miles (Fig. 2).<br />

With<strong>in</strong> <strong>the</strong> area of Reservoir B <strong>the</strong>re are numerous thick sands<br />

below <strong>the</strong> top of <strong>the</strong> geopressured zone.<br />

The "10,000 foot" sand is<br />

below <strong>the</strong> top of <strong>the</strong> geopressured zone, and is laterally cont<strong>in</strong>uous<br />

with<strong>in</strong> <strong>the</strong> area.<br />

<strong>Additional</strong>ly, this sand has <strong>the</strong> lowest reported<br />

sal<strong>in</strong>ity (4,000 ppm CI) of any of <strong>the</strong> sands <strong>for</strong> which data are<br />

available.<br />

The top of <strong>the</strong> sand occurs at 9,550 feet on <strong>the</strong> west<br />

side of <strong>the</strong> reservoir and at 10,360 feet on <strong>the</strong> east side. The dip<br />

is relatively flat across <strong>the</strong> top of <strong>the</strong> Weslaco high or "uplift,"<br />

although <strong>the</strong> dip angle beg<strong>in</strong>s to <strong>in</strong>crease markedly at greater<br />

depth.<br />

II-II

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