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TitleWorld sedimentary exhalative (Sedex) deposit database
DownloadDownloads
AuthorSangster, D F
SourceGeological Survey of Canada, Open File 7773, 2015, 7 pages, https://doi.org/10.4095/296423 (Open Access)
Year2015
PublisherNatural Resources Canada
Documentopen file
Lang.English
Mediadigital; on-line
RelatedThis publication is related to the following publications
File formatreadme
File formatpdf; rtf; mdb; sql; kmz; mxd; htm; txt; shp; lyr
ProvinceBritish Columbia; Alberta; Saskatchewan; Manitoba; Ontario; Quebec; New Brunswick; Nova Scotia; Prince Edward Island; Canada; Yukon; Northwest Territories; Nunavut; Newfoundland and Labrador
NTS1; 2; 3; 10; 11; 12; 13; 14; 15; 16; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 30; 31; 32; 33; 34; 35; 36; 37; 38; 39; 40; 41; 42; 43; 44; 45; 46; 47; 48; 49; 52; 53; 54; 55; 56; 57; 58; 59; 62; 63; 64; 65; 67; 66; 68; 69; 72; 73; 74; 75; 76; 77; 78; 79; 82; 83; 85; 84; 86; 87; 88; 89; 92; 93; 94; 95; 96; 97; 98; 99; 102; 103; 104; 105; 106; 107; 114; 115; 116; 117; 120; 340; 560
AreaWorld
Lat/Long WENS-180.0000 180.0000 90.0000 -90.0000
Subjectseconomic geology; sedimentary ore deposits; data collections; mineral deposits; mineral occurrences; reserve estimates; production; lithology; sedex; sedex deposits; Cenozoic; Mesozoic; Paleozoic; Proterozoic; Precambrian
Illustrationstables
ProgramDirector office, GSC Central Canada Division, GSC Central Canada Division
Released2015 05 27
Summary(Plain Language Summary, not published)
The spatial distribution and most significant geological attributes of the world's largest sedimentary exhalative (Sedex) lead-zinc metallic mineral deposits and mineral districts are depicted in this data set. These deposits are hosted by marine sedimentary rocks, such as shale, greywacke, and carbonate, and are thought to have originated because of the submarine venting of hydrothermal fluid rich in zinc and lead.
GEOSCAN ID296423