Fourth level Play Fairway Analysis Fifth level Shelburne Delta

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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

Thank you

Fourth level Play Fairway Analysis Fifth level Shelburne Delta

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