GEOSCAN Search Results: Fastlink

GEOSCAN Menu


TitleU-Pb geochronology of volcanic and plutonic rocks from the White Hills Lake to Meadowbank River area, Rae Province, Nunavut, Canada
DownloadDownloads
 
LicencePlease note the adoption of the Open Government Licence - Canada supersedes any previous licences.
AuthorDavis, W JORCID logo; Zaleski, E; Emon, Q
SourceGeological Survey of Canada, Open File 8766, 2021, 11 pages, https://doi.org/10.4095/327936 Open Access logo Open Access
Image
Year2021
PublisherNatural Resources Canada
Documentopen file
Lang.English
Mediaon-line; digital
File formatreadme
File formatpdf; rtf; xlsx (Microsoft® Excel®)
ProvinceNunavut
NTS55M/11; 55M/12; 55M/13; 55M/14; 56D/03; 56D/04; 56D/05; 56D/06; 65P/09; 65P/10; 65P/15; 65P/16; 66A/01; 66A/02; 66A/07; 66A/08
AreaKivalliq; Woodburn Lake; White Hills Lake; Meadowbank River
Lat/Long WENS -96.7500 -95.4167 65.3667 64.5833
Subjectsgeochronology; economic geology; Science and Technology; Nature and Environment; radiometric dating; uranium lead dating; zircon dates; mass spectrometer analysis; bedrock geology; lithology; igneous rocks; volcanic rocks; felsic volcanic rocks; tuffs; porphyries; intrusive rocks; granites; structural features; faults; folds; Archean; Canadian Shield; Rae Province; Ketyet River Group; Woodburn Lake Group; Halfway Hills Thrust; Meadowbank River Fault; Meadowbank River Thrust; White Hills Thrust; Whitehills Belt; Neoarchean; Mesoarchean; Precambrian
Illustrationslocation maps; geoscientific sketch maps; Concordia diagrams; tables
ProgramGEM2: Geo-mapping for Energy and Minerals Rae Province
ProgramWestern Churchill NATMAP Project
Released2021 03 23
Summary(Plain Language Summary, not published)
This publication presents data to support age interpretations for volcanic and plutonic rocks from the Woodburn Lake area, north of Baker Lake in the Kivalliq district of Nunavut. The rocks form part an ancient volcanic sequence that formed 2.7 billion years ago and host important gold deposits (e.g. Meadowbank mine). The ages were determined using natural radioactive decay of Uranium to Lead within the mineral zircon, an important accessory mineral that crystallized at the same time as the rock. The data can be used to understand when and how the rocks in this area formed and how they may correlate to other units in the area in order to develop better geological models.
GEOSCAN ID327936

 
Date modified: