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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Banks Island
The Devonian clastic wedge and underlying strata of southwestern Canadian Arctic Archipelago: stratigraphic revisions
Paralava and clinker from the Canadian Arctic: a record of combustion metamorphism dating back to the late Miocene
Glass fission-track ages, composition, and origin of tephra beds in the Upper Cretaceous Kanguk Formation, Banks Island, Arctic Canada
Investigating the Paleozoic–Mesozoic low-temperature thermal history of the southwestern Canadian Arctic: insights from (U–Th)/He thermochronology
U-Pb and Hf isotope analysis of detrital zircons from Paleozoic strata of the southern Alexander terrane (southeast Alaska)
Evidence from shark teeth for a brackish Arctic Ocean in the Eocene greenhouse
Petroleum Systems and Seismic Expression of Exploration Plays, Canadian Arctic Margin, Beaufort Sea
Abstract The Canadian Arctic margin, from the Alaska/ Canada boundary north-northeastward almost 1,000 km to the north of Banks Island, represents one of the largest sedimentary wedges in the world. With primary input from the Mackenzie River, the margin appears to have all the necessary components of a “world-class” petroleum province: possibilities of structural and stratigraphic traps, multiple potential source rocks, an abundance of potential reservoirs and seals, and timely migration resulting in almost 50 hydrocarbon accumulations discovered to date. However, lack of a large enough discovery to warrant commercial production has resulted in exploration being limited only to the shallow parts of the Mackenzie River Delta (water depths <40 m). Interpretation of recent, long-offset (9 km), deep (18-sec recording), prestack-depth migrated (PSDM to 40 km) data has resulted in extending the petroleum potential to deeper waters and to areas away from the delta. Industry has recognized this potential by acquiring leases beyond the shallow waters, but the full potential of the area will only be realized by new exploratory drilling.
A summertime rainy season in the Arctic forests of the Eocene
MOLECULAR PRESERVATION OF CENOZOIC CONIFER FOSSIL LAGERSTÄTTEN FROM BANKS ISLAND, THE CANADIAN ARCTIC
Lower Paleozoic Thermal Maturity and Hydrocarbon Potential of the Canadian Arctic Archipelago
Magnetostratigraphy of Quaternary and late Tertiary sediments on Banks Island, Canadian Arctic Archipelago
The Sangamonian and early Wisconsinan glacial record in the western Canadian Arctic
Widespread till sheets, glacial lake and glacial-marine sediments on Banks, Victoria, and Melville islands, and on the Beaufort Sea Coastal Plain of the Canadian mainland, may record a late Pleistocene glacial advance which extended to the area as early as the Sangamonian (broad sense) to early Wisconsinan. These sediments overlie beds of interglacial character and underlie in places nonglacial deposits, which have provided both nonfinite and finite ages, and glacial sediments of unquestionable late Wisconsinan age. In other places only a single till sheet is observed between the last interglacial and Holocene sediment suites. Although some workers have argued that the glacial units mentioned above are all late Wisconsinan, stratigraphic, paleoecologic, and chronologic data ( 14 C, Th/U, and amino acid analyses), from several localities, indicate that the glacial sediments are of likely Sangamonian (broad sense) to early Wisconsinan age and that the nonglacial beds underlying or overlying these date respectively from the Sangamonian and middle Wisconsinan. The dispersal centre during the ice advance was situated, as during other advances in northwestern Canada, west of Hudson Bay. The ice generally extended further during the Sangamonian (broad sense)/early Wisconsinan than the late Wisconsinan but not as far as it did during the early and middle Pleistocene. To help resolve apparent incongruities in interpretation of the late Pleistocene deposits and ice limits it is postulated that extensive Keewatin Sector Ice of the Laurentide Ice Sheet may have first advanced in northwestern Canada during the Sangamonian (broad sense)/early Wisconsinan and remained there until it finally disappeared in the late Wisconsinan.