Sedimentary basins and basement highs beneath the polar shelf north of Axel Heiberg and Meighen Islands

D A Forsyth, I Asudeh, D White, R Jackson, R A Stephenson, A F Embry, M Argyle

Research output: Contribution to journalArticle

8 Citations (Scopus)

Abstract

A seismic refraction program was carried out on the northeastern polar continental shelf north of Axel Heiberg and Meighen islands, Five distinct velocity units were identified throughout the area, The deepest unit, velocity unit 1, has velocities of 8.2 km/sec and represents the ultramafic, uppermost mantle, The top of this unit is the MOHO and it is about 25 km deep on the inner shelf and rises to 20 km on the outer shelf. The next velocity unit (2) has velocities of 6.6 to 6.8 km/sec and correlates well with the crystalline lower crust.

Velocity unit 3 is characterized by velocities of 5.9 to 6.2 km/sec and is interpreted to consist primarily of highly indurated elastic and carbonate strata, volcanics and intrusives of the highly deformed, late Proterozoic to early Paleozoic Franklinian Basin. Along the shelf edge this unit may also encompass Lower Cretaceous volcanic flows and Jurassic-Cretaceous strata which are extensively intruded by sills and dykes. The top of this unit is considered to be "basement".

Velocity unit 4 has velocities between 4.3 and 5.3 km/sec and is interpreted to consist mainly of mid Jurassic to Paleogene deltaic to basinal elastic strata, This unit is up to 10 km thick and occurs throughout the study area except over an offshore extension of the Princess Margaret Arch on the inner shelf and the crest of a prominent shelf edge high. The strata encompassed by this unit are likely deformed by folds and faults generated during the early Tertiary Eurekan Orogeny.

Velocity unit 5 has velocities of 1.9 to 3.4 km/sec and probably comprises the undeformed Neogene succession, This unit is a few kilometres thick over much of the shelf and may include buried Upper Cretaceous-Paleogene strata on the inner shelf.

The potential of the deformed Cretaceous-Paleogene succession to contain hydrocarbons is high but the presence of the Arctic ice pack over the area hampers traditional exploration.

Original languageEnglish
Pages (from-to)12-29
Number of pages18
JournalBulletin of Canadian Petroleum Geology
Volume46
Issue number1
Publication statusPublished - Mar 1998

Keywords

  • crustal structure
  • Beaufort Sea
  • synthetic seismograms
  • Arctic Archipelago
  • Alpha-Ridge
  • margin
  • stratigraphy
  • evolution
  • Canada

Cite this

Sedimentary basins and basement highs beneath the polar shelf north of Axel Heiberg and Meighen Islands. / Forsyth, D A ; Asudeh, I ; White, D ; Jackson, R ; Stephenson, R A; Embry, A F ; Argyle, M .

In: Bulletin of Canadian Petroleum Geology, Vol. 46, No. 1, 03.1998, p. 12-29.

Research output: Contribution to journalArticle

Forsyth, DA, Asudeh, I, White, D, Jackson, R, Stephenson, RA, Embry, AF & Argyle, M 1998, 'Sedimentary basins and basement highs beneath the polar shelf north of Axel Heiberg and Meighen Islands' Bulletin of Canadian Petroleum Geology, vol. 46, no. 1, pp. 12-29.
Forsyth, D A ; Asudeh, I ; White, D ; Jackson, R ; Stephenson, R A ; Embry, A F ; Argyle, M . / Sedimentary basins and basement highs beneath the polar shelf north of Axel Heiberg and Meighen Islands. In: Bulletin of Canadian Petroleum Geology. 1998 ; Vol. 46, No. 1. pp. 12-29.
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T1 - Sedimentary basins and basement highs beneath the polar shelf north of Axel Heiberg and Meighen Islands

AU - Forsyth, D A

AU - Asudeh, I

AU - White, D

AU - Jackson, R

AU - Stephenson, R A

AU - Embry, A F

AU - Argyle, M

PY - 1998/3

Y1 - 1998/3

N2 - A seismic refraction program was carried out on the northeastern polar continental shelf north of Axel Heiberg and Meighen islands, Five distinct velocity units were identified throughout the area, The deepest unit, velocity unit 1, has velocities of 8.2 km/sec and represents the ultramafic, uppermost mantle, The top of this unit is the MOHO and it is about 25 km deep on the inner shelf and rises to 20 km on the outer shelf. The next velocity unit (2) has velocities of 6.6 to 6.8 km/sec and correlates well with the crystalline lower crust.Velocity unit 3 is characterized by velocities of 5.9 to 6.2 km/sec and is interpreted to consist primarily of highly indurated elastic and carbonate strata, volcanics and intrusives of the highly deformed, late Proterozoic to early Paleozoic Franklinian Basin. Along the shelf edge this unit may also encompass Lower Cretaceous volcanic flows and Jurassic-Cretaceous strata which are extensively intruded by sills and dykes. The top of this unit is considered to be "basement".Velocity unit 4 has velocities between 4.3 and 5.3 km/sec and is interpreted to consist mainly of mid Jurassic to Paleogene deltaic to basinal elastic strata, This unit is up to 10 km thick and occurs throughout the study area except over an offshore extension of the Princess Margaret Arch on the inner shelf and the crest of a prominent shelf edge high. The strata encompassed by this unit are likely deformed by folds and faults generated during the early Tertiary Eurekan Orogeny.Velocity unit 5 has velocities of 1.9 to 3.4 km/sec and probably comprises the undeformed Neogene succession, This unit is a few kilometres thick over much of the shelf and may include buried Upper Cretaceous-Paleogene strata on the inner shelf.The potential of the deformed Cretaceous-Paleogene succession to contain hydrocarbons is high but the presence of the Arctic ice pack over the area hampers traditional exploration.

AB - A seismic refraction program was carried out on the northeastern polar continental shelf north of Axel Heiberg and Meighen islands, Five distinct velocity units were identified throughout the area, The deepest unit, velocity unit 1, has velocities of 8.2 km/sec and represents the ultramafic, uppermost mantle, The top of this unit is the MOHO and it is about 25 km deep on the inner shelf and rises to 20 km on the outer shelf. The next velocity unit (2) has velocities of 6.6 to 6.8 km/sec and correlates well with the crystalline lower crust.Velocity unit 3 is characterized by velocities of 5.9 to 6.2 km/sec and is interpreted to consist primarily of highly indurated elastic and carbonate strata, volcanics and intrusives of the highly deformed, late Proterozoic to early Paleozoic Franklinian Basin. Along the shelf edge this unit may also encompass Lower Cretaceous volcanic flows and Jurassic-Cretaceous strata which are extensively intruded by sills and dykes. The top of this unit is considered to be "basement".Velocity unit 4 has velocities between 4.3 and 5.3 km/sec and is interpreted to consist mainly of mid Jurassic to Paleogene deltaic to basinal elastic strata, This unit is up to 10 km thick and occurs throughout the study area except over an offshore extension of the Princess Margaret Arch on the inner shelf and the crest of a prominent shelf edge high. The strata encompassed by this unit are likely deformed by folds and faults generated during the early Tertiary Eurekan Orogeny.Velocity unit 5 has velocities of 1.9 to 3.4 km/sec and probably comprises the undeformed Neogene succession, This unit is a few kilometres thick over much of the shelf and may include buried Upper Cretaceous-Paleogene strata on the inner shelf.The potential of the deformed Cretaceous-Paleogene succession to contain hydrocarbons is high but the presence of the Arctic ice pack over the area hampers traditional exploration.

KW - crustal structure

KW - Beaufort Sea

KW - synthetic seismograms

KW - Arctic Archipelago

KW - Alpha-Ridge

KW - margin

KW - stratigraphy

KW - evolution

KW - Canada

M3 - Article

VL - 46

SP - 12

EP - 29

JO - Bulletin of Canadian Petroleum Geology

JF - Bulletin of Canadian Petroleum Geology

SN - 0007-4802

IS - 1

ER -