GEOSCAN Search Results: Fastlink


TitleTectonostratigraphy and allochthonous salt tectonics of Axel Heiberg Island, central Sverdrup Basin, Arctic Canada
AuthorHarrison, J C; Jackson, M P A
SourceGeological Survey of Canada, Bulletin no. 607, 2014, 134 pages,
Alt SeriesTexas Bureau of Economic Geology , Report of Investigations 279
PublisherNatural Resources Canada
PublisherBureau of Economic Geology (Austin, TX, US)
Mediadigital; on-line; paper
File formatpdf
NTS59E/13; 59E/14; 59F/15; 59F/16; 59G; 59H/03; 59H/04; 59H/05; 59H/06; 59H/12
AreaAxel Heiberg Island,
Lat/Long WENS-94.2500 -89.7500 79.7500 78.7500
Subjectstectonics; stratigraphy; structural geology; sedimentology; paleontology; geophysics; tectonic evolution; tectonic environments; tectonic interpretations; tectonic elements; tectonic history; rifts; sedimentary basins; basin analysis; basins; structural analyses; structural features; folds; faults; faults, thrust; structural interpretations; coal; bedrock geology; biostratigraphy; seismic profiles; stratigraphic correlations; stratigraphic analyses; grabens; wells; hydrocarbon generation; diapirs; Sverdrup Basin; Borup Fiord Formation; Otto Fiord Formation; Hare Fiord Formation; Trappers Cove Formation; Blind Fiord Formation; Blaa Mountain Group; Heiberg Formation; Awingak Formation; Deer Bay Formation; Isachsen Formation; Christopher Formation; Macdougall Point Member; Hassel Formation; Bastion Ridge Formation; Strand Fiord Formation; Kanguk Formation; Expedition Formation; Strand Bay Formation; Iceberg Bay Formation; Jameson Bay Formation; McConnell Island Formation; Ringnes Formation; Cenozoic; Triassic; Jurassic; Cretaceous; Mesozoic; Quaternary; Tertiary; Permian; Carboniferous; Mississippian; Devonian; Pennsylvanian; Silurian; Proterozoic
Illustrationslocation maps; stratigraphic correlations; stratigraphic sections; photographs; cross-sections; histograms
ProgramRae Province Project Management, GEM2: Geo-mapping for Energy and Minerals
LinksOrder // Commander
Released2014 10 06
AbstractAxel Heiberg Island (northern Nunavut) contains the thickest Mesozoic section in Sverdrup Basin. The approximately 370 km long island is second only to Iran in its concentration of exposed diapirs. Forty-six diapirs of Carboniferous evaporites and associated minibasins are impressively exposed on the island. Regional anticlines, which formed during the Paleogene Eurekan Orogeny, trend roughly north on a regular approximately 20 km wavelength and probably detach on the autochthonous Carboniferous Otto Fiord Formation evaporites. These evaporites comprise halite overlain by thick anhydrite containing thin limestone beds. Unlike the rest of the island, a 60 km wide area, known as the wall-and-basin region, has bimodal fold trends and irregular (<10 km) fold wavelengths. Here, crooked, narrow walls of superficially gypsified anhydrite crop out in tight anticline cores, which are separated by wider synclinal minibasins. We interpret the wall-andbasin region to detach on a shallow, partly exposed canopy of coalesced allochthonous evaporite sheets. This inference is based on four lines of evidence: 1) a halving of fold wavelength relative to folds outside the wall-and-basin region, 2) the exposure of anomalously young strata of Paleogene and Late Cretaceous age, 3) the occurrence of clustered equant minibasins having similarities to those in the northern Gulf of Mexico, and 4) a strikingly uniform level of piercement pointing to a stratiform allochthonous source layer. A canopy would require an evaporite depocentre, which may have ponded in a sinistral pull-apart basin of Carboniferous age. Strata record a salt-tectonic history spanning the Late Triassic (Norian) epoch to the Paleogene period. Stratigraphic thinning against diapirs and angular unconformities up to 90° indicate mild regional shortening in which diapiric roof strata were bulged up and flanking strata steepened. This bulging culminated during Hauterivian times, when diapiric evaporites broke out and coalesced at the surface to form a canopy. As the canopy was buried, it yielded second-generation diapirs, which rose between minibasins subsiding into the canopy. A consistent high emplacement level indicates that all exposed diapirs inside the wall-and-basin region rose from the canopy. In contrast, diapirs along the wall-and-basin margins were sourced in autochthonous salt as first-generation diapirs. Apart from the large diapir-centred unconformities, Jurassic-Cretaceous depositional evidence of salt tectonics also includes submarine debris flows and boulder conglomerates shed from at least three emergent diapirs. The report area's geological history includes six main tectonostratigraphic phases in the wider Arctic area, beginning with Carboniferous rifting and ending with the Paleogene Eurekan Orogeny. Extreme local relief, tectonic slide blocks, steep talus fans, and subaerial debris flows suggest that many wall-and-basin diapirs continue to rise today. Freeboard calculations suggest that the rise of diapirs having surface relief of even 400 m could be driven purely by gravitational loading, but additional mild tectonic shortening cannot be ruled out. The Axel Heiberg canopy is one of only three known exposed evaporite canopies, each revealed at a different structural level: above the canopy (Axel Heiberg), through the canopy (Great Kavir, Iran), and possibly beneath a canopy (Sivas Basin, Turkey).
Summary(Plain Language Summary, not published)
The Sverdrup Basin in the Canadian Arctic Islands is a well known repository for natural gas and some oil. Closely associated with the known hydrocarbons are bodies of rock salt that have moved up into younger rocks as the basin was filled with sediment. The present paper describes the unusual salt structures of western Axel Heiberg Island and the sediments within which the salt is found. The case is made for sheets of salt emplaced into Cretaceous strata and the possibility that these structures may contain as yet undiscovered oil and gas.