CallForBidsNF00-1 - Jeanne d'Arc, South Whale, Magdalen Basins

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4610’ O 450’ O O Parcel 5 Request For Bids Parcels Page 24 Location: Carson / Bonnition Basin Parcel Area: 215,875 hectares Water depth: >1000 m Released Seismic Data: 2920.01 km Data Vintages: 1966 –1983 Play Types: - Base of Tertiary fans and turbidites - Cretaceous and Jurassic sands in tilted fault blocks This line shows a basement high to the north and west with little or no overlying Jurassic or Cretaceous sediments. Thick Tertiary sediment in the southeastern portion of the parcel may contain turbidite deposits at the base of the slope break. Below these features, a deep seated fault block may contain Lower Cretaceous and Jurassic sections. O -47 00’ O -47 00’ # 5 # 7 # 4 # 6 O -49 00’ O 46 10’ Cormorant N-83 RELEASED SEISMIC DATA (POST 1980) and WELL LOCATIONS CARSON BONNITION BASIN, OFFSHORE NEWFOUNDLAND UTM 22 Projection (NAD 83) St. George J-55 Skua E-41 20 km T. Bennett 4-Apr-2000 -49 00’ 0
Parcel 6 Page 25 Request For Bids Parcels NW 0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 0 kilometres 10 20 30 40 50 60 SE 0.0 1.0 2.0 3.0 4.0 5.0 6.0 TWO-WA TIME(seco s) Y n BASEMENT Salt Iroquois PARCEL 6 Base of Tertiary Fan JURASSIC Seabed Basement Ridge TERTIARY Upper Cretaceous Subcrop CRETACEOUS 7.0 O -47 00’ O -49 00’ Note: Program # 8620-S014-008E SEISMIC LINE 83-2642 O 46 10’ # 6 # 4 # 7 # 5 0 Cormorant N-83 Skua E-41 St. George J-55 20 km RELEASED SEISMIC DATA (POST 1980) and WELL LOCATIONS CARSON BONNITION BASIN, OFFSHORE NEWFOUNDLAND UTM 22 Projection (NAD 83) T. Bennett 4-Apr-2000 Location: Carson / Bonnition Basin Parcel Area: 188,420 hectares Water depth: 100 - >1000 m Released Seismic Data: 2063.28 km Data Vintages: 1971 –1985 Play Types: - Base of Tertiary fans and turbidites - Cretaceous and Jurassic sands in tilted fault blocks - Pinch out of Jurassic sands and carbonates against the Base of Tertiary unconformity and over the basement high on the NW end of the line This line clearly shows the high terrace along the western part of the Carson Basin dropping off to the east where a thick Jurassic section is preserved. No Lower Cretaceous has been interpreted to be present in this part of the Carson Basin. The Jurassic section has been deformed by salt movement resulting in steeply dipping beds that terminate against the base of Tertiary unconformity providing the opportunity for stratigraphic traps. Overlying the Jurassic section, fans and turbidite deposits are interpreted in the Lower Tertiary. To the east of the basement ridge, tilted fault blocks provide the opportunity for structural traps within the Jurassic.
Page 1 and 2: Department of Mines and Energy Gove
Page 3 and 4: Department of Mines and Energy Offs
Page 5 and 6: INTRODUCTION Page 3 Fourteen parcel
Page 7 and 8: Page 5 STRATEGIC LOCATION The Hiber
Page 9 and 10: Page 7 INDUSTRIAL INFRASTRUCTURE A
Page 11 and 12: Page 9 INFRASTRUCTURE North Atlanti
Page 13 and 14: -53°00' -48°00' 0 100KM BRUNSWICK
Page 15 and 16: EGRET Page 13 GEOLOGICAL FRAMEWORK
Page 17 and 18: Page 15 GEOLOGICAL FRAMEWORK Carson
Page 19 and 20: GEOLOGICAL FRAMEWORK The presence o
Page 21 and 22: Section 4 Page 19 Request For Bids
Page 23 and 24: Parcel 2 Page 21 Request For Bids P
Page 25: 4610’ O 45 0’ O Parcel Parcel 4
Page 29 and 30: O -52 0’ O 43 0’ Parcel 8 Reque
Page 31 and 32: Parcel 10 Parcel 10 Request For Bid
Page 33 and 34: O -5200’ O 43 0’ Parcel 11 Requ
Page 35 and 36: -5 2 0 0 ’ O 430’ O Parcel 13 R
Page 37 and 38: Section 5 HOW TO MAKE A BID Page 35
Page 39 and 40: Page 37 FISCAL REGIMES AND TAXATION
Page 41 and 42: Section 8 Page 39 Bibliography, End
Page 43 and 44: Appendix A Parcel 5 Program Number
Page 45 and 46: HIBERNIA 1 1 TERRA NOVA HEBRON WHIT

CallForBidsNF00-1 - Jeanne d'Arc, South Whale, Magdalen Basins

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