CallForBidsNF00-1 - Jeanne d'Arc, South Whale, Magdalen Basins
CallForBidsNF00-1 - Jeanne d'Arc, South Whale, Magdalen Basins
CallForBidsNF00-1 - Jeanne d'Arc, South Whale, Magdalen Basins
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O<br />
-52 0’<br />
O 43 0’<br />
Parcel 8<br />
Request For Bids Parcels<br />
Page 27<br />
PARCEL 8<br />
O<br />
-5200’<br />
RazorbilF-54<br />
GanetO-54<br />
O<br />
45 00’<br />
PetrelĀ62 Merganser I-60<br />
#8<br />
#9<br />
#10<br />
#1<br />
O<br />
44 00’<br />
#12 #13<br />
Kittiwake P-11<br />
Puffin B-90<br />
Narwhal F-99<br />
Tern A-68 Shearwater J-20<br />
Malard<br />
M-45<br />
0<br />
20 km<br />
Brant P-87<br />
Gull F-72<br />
Heron H-73<br />
Tors Cove<br />
D-52<br />
Heron<br />
J-72<br />
RELEASED SEISMIC DATA (POST 1980)<br />
and WELL LOCATIONS<br />
CARSON BONNITION BASIN,<br />
OFFSHORE NEWFOUNDLAND<br />
UTM 22 Projection (NAD 83)<br />
T. Bennett<br />
4-Apr-2000<br />
Carbonate<br />
Bank<br />
Location: <strong>South</strong> <strong>Whale</strong> Basin<br />
Parcel Area: 220,140 hectares<br />
Water depth: 100 m<br />
Released Seismic Data: 6787.59 km<br />
Data Vintages: 1964 –1985<br />
Play Types:<br />
- Drape of Cretaceous sands over<br />
Jurassic fault blocks and salt cored<br />
structures<br />
- Cretaceous and Jurassic sands in tilted<br />
fault blocks or over salt cored structures<br />
- Faulted Jurassic structures below salt<br />
diapirs<br />
- Prograding Jurassic sands in<br />
stratigraphic traps pinched out against<br />
the Base of Cretaceous unconformity<br />
- Jurassic carbonate bank porosity in<br />
structural and stratigraphic traps<br />
Thick sections of reservoir quality sands were<br />
encountered at the Mississauga level in the two wells<br />
drilled on this parcel. Kittiwake P-11 was drilled adjacent<br />
to a salt dome which would appear to have had very late<br />
movement as it breaches the sea bed. Puffin B-90 tested a<br />
fault play which it appears was not sealed across the<br />
fault. Potential plays exist where gentle roll overs can be<br />
mapped at the Mississauga - as evident between<br />
kilometres 5 and 15. Jurassic carbonates draped over<br />
Windsor salt and subbcropping against the Base of<br />
Cretaceous unconformity may provide deeper targets.