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TitleGeochemical data of Yukon-Tanana and Slide Mountain terranes and their successor rocks in Yukon and northern British Columbia
LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorRyan, J J; Zagorevski, AORCID logo; Piercey, S J
SourceGeological Survey of Canada, Open File 8500, 2018, 11 pages, Open Access logo Open Access
PublisherNatural Resources Canada
Documentopen file
Mediaon-line; digital
File formatreadme
File formatpdf (Adobe® Reader®); rtf; xlsx (Microsoft® Excel®); xls (Microsoft® Excel®)
ProvinceYukon; British Columbia
NTS104I; 104J; 104K; 104L; 104M; 104N; 104O; 104P; 105; 114; 115
AreaWhitehorse; Stewart River; McQuesten; Stevenson Ridge; Mount Nansen; Klaza River
Lat/Long WENS-141.0000 -128.0000 64.0000 58.0000
Subjectsgeochemistry; geochemical analyses; whole rock analyses; major element analyses; trace element analyses; bedrock geology; lithology; lithostratigraphy; x-ray fluorescence analyses; spectrometric analyses; Paleocene; Yukon-Tanana Terrane; Slide Mountain Terrane; Canadian Cordillera; Intermontane Belt; Intermontane Superterrane; Phanerozoic; Cenozoic; Tertiary; Mesozoic; Cretaceous; Triassic; Paleozoic
Illustrationsgeoscientific sketch maps; location maps; geochemical plots; ternary diagrams
ProgramGEM2: Geo-mapping for Energy and Minerals Western Cordillera, Devonian and Permian structural architecture
ProgramAncient Pacific Margin NATMAP Project
Released2018 12 06
Summary(Plain Language Summary, not published)
Geochemical data presented in this open file release, have been collected in southern Yukon and northern British Columbia over a sixteen year period from 2000 to 2016 as part of regional mapping projects conducted under the auspices of the Geological Survey of Canada's Ancient Pacific Margin (NATMAP) and Geo-mapping for Energy and Minerals (GEM) programs. The data includes major and trace element analyses for some 818 rock samples, from a wide range of geological units that range in age from pre-Late Devonian to Paleocene.

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