GEOSCAN Search Results: Fastlink

GEOSCAN Menu


TitleA new regional mapping project in Vernon map area, British Columbia
DownloadDownload (whole publication)
LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorThompson, R I; Daughtry, K L
SourceCordillera and Pacific Margin/Cordillère et marge du Pacifique; by Geological Survey of Canada; Geological Survey of Canada, Current Research no. 1994-A, 1994 p. 117-122, https://doi.org/10.4095/193629 Open Access logo Open Access
Year1994
PublisherNatural Resources Canada
Documentserial
Lang.English
Mediapaper; on-line; digital
RelatedThis publication is contained in Geological Survey of Canada; (1994). Cordillera and Pacific Margin, Geological Survey of Canada, Current Research no. 1994-A
File formatpdf
ProvinceBritish Columbia
NTS82L/03; 82L/06
AreaVernon; Lavington; Okanagan Lake
Lat/Long WENS-119.5000 -119.0000 50.5000 50.0000
Subjectsigneous and metamorphic petrology; structural geology; metallic minerals; industrial minerals; Eocene; faults; structural features; volcanic rocks; igneous rocks; porphyry deposits; volcanogenic deposits; sulphide deposits; skarn deposits; base metal deposits; mineral deposits; stratigraphic analyses; metasedimentary rocks; quartzites; schists; metavolcanic rocks; metamorphic rocks; limestones; conglomerates; breccias; sedimentary rocks; plutonic rocks; diorites; granodiorites; granites; ultramafic rocks; lithology; metallogeny; gold; silver; copper; molybdenum; gypsum; Quesnellia Terrane; Kootenay Terrane; Windermere Group; Jurassic; Triassic; Tertiary
Illustrationssketch maps
Released1994 02 01
AbstractIn Vernon map area (82L) at least two stratigraphic assemblages link Quesnel terrane, Kootenay terrane and undivided metamorphic assemblages: 1) a Windermere-like biotite/hornblende- feldspar-quartz assemblage; and 2) a carbonaceous schist, phyllite, argillite assemblage. Volcanic rocks, east of Vernon, thought to be Triassic and unconformable on older strata are likely part of an Eocene succession emplaced during crustal extension. Eocene crustal extension was distributed across a broad area along steeply dipping faults; the horizontal component across north Okanagan Valley amounts to a few kilometres. Metallic mineral deposit types include porphyry copper and molybdenum, Kuroko-type volcanogenic massive sulphide, skarn copper and gold, mesothermal gold, silver, and base metal veins, epithermal gold and silver veins and breccias, placer gold, and podiform chromite. Nonmetallic mineral occurrences include granite, sand and gravel, limestone, marble, gypsum, clay, asbestos, soapstone, coal, agate, opal, jasper, wollastonite, fluorite, palagonite, silica, and kyanite.
GEOSCAN ID193629

 
Date modified: