HORN RIVER BASIN Subsurface Aquifer ... - Geoscience BC
HORN RIVER BASIN Subsurface Aquifer ... - Geoscience BC HORN RIVER BASIN Subsurface Aquifer ... - Geoscience BC
d-92-H / 94-O-9 Gamma PE Density SP Resis DETRITAL ZONE • Extensive and intensive dolomitization at pre‐Cretaceous unconformity • Poor core and sample recovery • Poor log characterization –washed out
Regional fracturing (Giant Springs, Great Falls) DETRITAL ZONE OUTCROP ANALOGUE Madison Group, Northern Montana Solution breccia, dolomitization, recrystallization
- 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: Φ K Debolt Upper Rundle 25 m DETRI
- 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 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
d-92-H / 94-O-9<br />
Gamma PE Density SP Resis<br />
DETRITAL ZONE<br />
• Extensive and intensive dolomitization<br />
at pre‐Cretaceous unconformity<br />
• Poor core and sample recovery<br />
• Poor log characterization –washed out
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