HORN RIVER BASIN Subsurface Aquifer ... - Geoscience BC
HORN RIVER BASIN Subsurface Aquifer ... - Geoscience BC HORN RIVER BASIN Subsurface Aquifer ... - Geoscience BC
ISOPACH MATTSON FORMATION • Present only in Bovie Fault Zone, thickens rapidly westward • May be aquifer target in extreme western part of shale gas area
Debolt clast GETHING FORMATION • Fills south‐north trending valley on eastern flank of HRB • incises eastern margin of Debolt • Abundant poorly‐sorted detritus • Variable reservoir quality, but some good rock in most wells • Hydrodynamic connection with Debolt
- 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 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: Mattson Formation (Jackfish Gap, Yu
- Page 25 and 26: CHINKEH FORMATION • Fluvial to ma
- Page 27 and 28: HORN RIVER BASIN AQUIFER CHARACTERI
- Page 29 and 30: NET POROUS ISOPACH MATTSON FORMATIO
- Page 31 and 32: POROSITY ‐ THICKNESS “DETRITAL
- Page 33 and 34: HORN RIVER BASIN AQUIFER CHARACTERI
- 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 39 and 40: HORN RIVER BASIN AQUIFER CHARACTERI
- Page 41: HORN RIVER BASIN Subsurface Aquifer
Debolt clast<br />
GETHING FORMATION<br />
• Fills south‐north trending valley on eastern<br />
flank of HRB<br />
• incises eastern margin of Debolt<br />
• Abundant poorly‐sorted detritus<br />
• Variable reservoir quality, but some good<br />
rock in most wells<br />
• Hydrodynamic connection with Debolt
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