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HORN RIVER BASIN Subsurface Aquifer ... - Geoscience BC

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Φ K<br />

25 m<br />

Debolt<br />

RUNDLE / DEBOLT<br />

• Correlated on flooding surface markers<br />

in Horn River Basin<br />

• Elkton / Shunda cannot be carried with<br />

confidence from southern areas<br />

• Stacked shoaling‐upward carbonate<br />

cycles form carbonate platform<br />

• dominantly mudstones to wackestones /<br />

packstones; little primary porosity<br />

• upper parts of cycles are dolomitized in<br />

middle of platform, in isolated wells

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