GEOSCAN Search Results: Fastlink

GEOSCAN Menu


TitleGeology, Ulukhaktok, Victoria Island, Northwest Territories
DownloadDownloads
 
LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorBédard, J H; Rainbird, R HORCID logo
SourceGeological Survey of Canada, Canadian Geoscience Map 190, 2015, 1 sheet, https://doi.org/10.4095/297279 Open Access logo Open Access
Image
Year2015
PublisherNatural Resources Canada
Editionprelim.
Documentserial
Lang.English
Maps1 map
Map Info.geological, bedrock and structural geology, 1:50,000
ProjectionUniversal Transverse Mercator Projection, UTM zone 11 (NAD83)
Mediaon-line; digital
RelatedNRCan photo(s) in this publication
File formatreadme
File formatpdf; shp; xml; rtf; xls
ProvinceNorthwest Territories
NTS87F/10; 87F/09SW; 87F/09NW
AreaVictoria Island; Qikiqtalik; Ingilraniq; Niviktuuyuq; Amundsen Gulf; Albert Islands; Tahiuyaq; Ulukhaktok
Lat/Long WENS-117.8500 -116.6000 70.7500 70.5000
Subjectsstratigraphy; structural geology; bedrock geology; sedimentary rocks; marine deposits; sandstones; dolostones; limestones; siltstones; shales; evaporites; carbonates; igneous rocks; volcanic rocks; dykes; sills; faults; intrusive rocks; structural features; Franklin Intrusions; Shaler Supergroup; Kilian Formation; Precambrian; Proterozoic
ProgramGEM: Geo-mapping for Energy and Minerals PGE/Base Metals - Victoria Island (NWT and Nunavut)
Released2015 12 14
AbstractNTS 87-F/9 and NTS 87-F/10 are underlain by the upper Kilian Formation of the Neoproterozoic Shaler Supergroup and mafic sills of the Franklin event. Shallowly east- and northeast-dipping strata define the nose and southern flank of the Holman Island Syncline. Carbonate, shale, and evaporitic rocks of the Kilian Formation are poorly exposed beneath capping sills or as thin contact-metamorphosed septa between sills. West of a major lake named Ingilraniq, a thick sill forms a high plateau disrupted by many north-south and east-west trending normal faults. A lower sill occupies the floor of some valleys. East of Ingilraniq, four thick sills separated by sedimentary septa form a series of cuestas. Resistant sills form prominent west-facing cliffs and mesas, and extend towards the east as diabase-floored plateaux.
Summary(Plain Language Summary, not published)
Map of 50k Sheet geology on Victoria island.
GEOSCAN ID297279

 
Date modified: