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» Fifth level Play Fairway Analysis – Shelburne Delta
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Topics
1. Previous research has indicated the likely
source of a sediment input point from the
George’s Bank Area “Shelburne Delta”.
2. Supported by DIONISIS modelling
indications of a sediment source into the SW
edge to the Scotian Slope are observed.
3. The Shelburne Delta is a viable source for
reservoir (sands) input to the Southwest
Scotian Slope during Logan Canyon and
possible Missisauga times.
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Shelburne Delta
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Shelburne Delta – Latest Jurassic
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Shelburne Delta – Early Cretaceous
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The George’s Bank Data
• 6000 km2
• reprocesses 2-D
• Consistent interpretation
• 3.5X12 km spacing
• *ties into PFA
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JEBCO Line 215 with Tie Lines to PFA
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JEBCO Line 215
400 m
s/tw
tt
5 km approx
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JEBCO Line 219 400 m
s/tw
tt
5 km approx
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Shelburne Delta, Mississauga Time
400 m
s/t
wtt
12 km
approx.
5 km approx
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Shelburne Delta, Logan Canyon Time
400 m
s/t
wtt
12 km
approx.
5 km approx
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PFA DIONISIS Model
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Perspective View of the Hauterivian
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Shelburne Delta
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Shelburne Delta Summary
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Shelburne Delta – Summary
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Shelburne Delta - Summary
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