HORN RIVER BASIN Subsurface Aquifer ... - Geoscience BC

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Φ K 50 ft 250’ to pKU Debolt Upper Rundle RUNDLE / DEBOLT • Correlated on flooding surface markers in Horn River Basin • Elkton / Shunda cannot be carried with confidence from southern areas • Stacked shoaling‐upward carbonate cycles form carbonate platform • dominantly mudstones to wackestones / packstones; little primary porosity • upper parts of cycles are dolomitized in middle of platform in isolated wells
ISOPACH MIDDLE RUNDLE • Subcrops east of HRB • Cannot distinguish from remainder of Rundle and Debolt to west
Page 1 and 2: HORN RIVER BASIN Subsurface Aquifer
Page 3 and 4: HORN RIVER BASIN AQUIFER CHARACTERI
Page 5 and 6: 94-J-11 94-P-14 94-I-11 HORN RIVER
Page 7 and 8: LIARD BASIN STRUCTURE TOP BANFF FM
Page 9 and 10: BANFF FORMATION • Distal carbonat
Page 11: Φ K 25 m Debolt RUNDLE / DEBOLT
Page 15 and 16: ISOPACH DEBOLT FORMATION • Pre‐
Page 17 and 18: Φ K Debolt Upper Rundle 25 m DETRI
Page 19 and 20: Regional fracturing (Giant Springs,
Page 21 and 22: Mattson Formation (Jackfish Gap, Yu
Page 23 and 24: Debolt clast GETHING FORMATION •
Page 25 and 26: CHINKEH FORMATION • Fluvial to ma
Page 29 and 30: NET POROUS ISOPACH MATTSON FORMATIO
Page 31 and 32: POROSITY ‐ THICKNESS “DETRITAL
Page 35 and 36: Bovie Fault Zone 30,000 Total Disso
Page 37 and 38: 27 e 6 m 3 / section 10 e 6 m 3 / s
Page 41: HORN RIVER BASIN Subsurface Aquifer

HORN RIVER BASIN Subsurface Aquifer ... - Geoscience BC

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