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Figures and Tables
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Figure 1, Top of the Minnekahta Structure Map
Structure map showing estimated position of down-to-the-east basement faults bounding the Donkey Creek and
Minny/East Donkey Creek features. The location of the cross section below is also shown.
Figure 2, Chorney to Recommended Drill Site Structural Cross Section
This structural interpretation is based on the discontinuity in dip rates that occurs between the area of the Chorney,
Klaenhammer, and Keeline wells, and the area of the Burrows 33-4 and Pursel wells, and the Recommended Drill Site. If
we project the dip rate at the top of the Minnekahta between the Keeline well and the Chorney well continuously to the
Recommended Drill Site, we would expect the Minnekahta to be 138 ft lower than the Chorney well. Instead, we find the
Minnekahta to be 29 ft higher than at the Chorney well. This gives us a discontinuity of 167 ft. We believe this discontinuity
is caused by an up-to-the-west basement fault of about the same magnitude as the one occurring on the east flank
of Donkey Creek.
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