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TitleStructural and depth contours of the Lower-Middle Aldridge Contact, east Kootenay region, southeastern British Columbia
DownloadDownloads
Authorde Kemp, E A; Schetselaar, E M
SourceGeological Survey of Canada, Open File 7903, 2015, 3 sheets, https://doi.org/10.4095/297429 (Open Access)
Image
Image
Image
Year2015
PublisherNatural Resources Canada
Documentopen file
Lang.English
Maps3 maps
Map Info.geological, 1:100,000
ProjectionUniversal Transverse Mercator Projection, UTM zone 11 (NAD83)
Mediaon-line; digital
File formatreadme
File formatpdf; rtf; shp; dxf; ts
ProvinceBritish Columbia
NTS82F/01; 82F/08; 82F/09; 82F/16; 82G/04; 82G/05; 82G/12; 82G/13
AreaKootenay; Kimberly
Lat/Long WENS-116.5000 -115.5000 50.0000 49.0000
Subjectseconomic geology; stratigraphy; structural geology; sedimentary ore deposits; structural features; structural analyses; faults; folds; mineral deposits; zinc; lead; mineralization; sedimentary basins; sedimentary rocks; igneous rocks; intrusions; Aldridge contact; McKay Group; Nicol Creek Formation; Van Creek Formation; Kitchener Formation; Creston Formation; Aldridge Formation; Paleozoic; Ordovician; Cambrian; Precambrian; Proterozoic
Illustrationsblock diagrams; models
ProgramSedimentary Exhalative Ore Systems, Targeted Geoscience Initiative (TGI-4)
Released2015 12 23
Summary(Plain Language Summary, not published)
Exploration for SEDEX deposits in the Purcell anticlinorium for >50 years has produced a large amount of regional geological, geochemical and geophysical data. 3D geological models are critical for discovery of buried mineral deposits, especially in well-explored areas like the Purcell anticlinorium, where good stratigraphic markers, a new digital map series and good topographic expression allow a regional 4-D restoration of the ore horizon. We now have the geologic and technical expertise to do this modelling for the more challenging regions away from a mine site and are also ready to enhance the way models are built with new tools that support more regional scale interpretation through estimation of spatial continuity of subsurface and surface geological features.
GEOSCAN ID297429