HORN RIVER BASIN Subsurface Aquifer ... - Geoscience BC

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HORN RIVER BASIN PRIMARY RESERVOIR UNITS • Mississippian carbonate platform • Local reservoir development within cycles • More consistent and higher‐ quality reservoir at upper surface in “Detrital” zone • Mattson sandstones (not shown) • to west in Bovie Fault Zone and Liard Basin • Cretaceous sandstones • Gething to east • Bluesky to southeast • Chinkeh (not shown) in Liard Basin
BANFF FORMATION • Distal carbonate mudstones • Limited clastic component (sltst –vf sst) to top • develops limited reservoir capacity where diagenetically enhanced at pre‐Cretaceous unconformity • NOT an aquifer target in Horn River Basin
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: LIARD BASIN STRUCTURE TOP BANFF FM
Page 11 and 12: Φ K 25 m Debolt RUNDLE / DEBOLT
Page 13 and 14: ISOPACH MIDDLE RUNDLE • Subcrops
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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