Title | Geology, Ulukhaktok, Victoria Island, Northwest Territories |
Download | Downloads |
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Licence | Please note the adoption of the Open Government Licence - Canada
supersedes any previous licences. |
Author | Bédard, J H; Rainbird, R H |
Source | Geological Survey of Canada, Canadian Geoscience Map 190, 2015, 1 sheet, https://doi.org/10.4095/297279 Open Access |
Image |  |
Year | 2015 |
Publisher | Natural Resources Canada |
Edition | prelim. |
Document | serial |
Lang. | English |
Maps | 1 map |
Map Info. | geological, bedrock and structural geology, 1:50,000 |
Projection | Universal Transverse Mercator Projection, UTM zone 11 (NAD83) |
Media | on-line; digital |
Related | NRCan photo(s) in this
publication |
File format | readme
|
File format | pdf; shp; xml; rtf; xls |
Province | Northwest Territories |
NTS | 87F/10; 87F/09SW; 87F/09NW |
Area | Victoria Island; Qikiqtalik; Ingilraniq; Niviktuuyuq; Amundsen Gulf; Albert Islands; Tahiuyaq; Ulukhaktok |
Lat/Long WENS | -117.8500 -116.6000 70.7500 70.5000 |
Subjects | stratigraphy; 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 |
Program | GEM: Geo-mapping for Energy and Minerals PGE/Base Metals - Victoria Island (NWT and Nunavut) |
Released | 2015 12 14 |
Abstract | NTS 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 ID | 297279 |
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