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TitleStructural evolution of the Woodburn Lake group in the area of the Meadowbank gold deposit, Nunavut
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AuthorHrabi, R B; Barclay, W A; Fleming, D; Alexander, R B
SourceGeological Survey of Canada, Current Research (Online) no. 2003-C27, 2003, 10 pages, https://doi.org/10.4095/214396
Year2003
PublisherNatural Resources Canada
Documentserial
Lang.English
Mediaon-line; digital; CD-ROM
RelatedThis publication is contained in Geological Survey of Canada; Geological Survey of Canada; (2004). Current Research 2003, January-December 2003, version 2, Geological Survey of Canada, Current Research no. 2003
File formatpdf
ProvinceNunavut
NTS56E/04; 66H/01
AreaWoodburn Lake; Meadowbank
Lat/Long WENS-96.0833 -95.9167 65.1667 65.0000
Subjectsregional geology; economic geology; Archean; bedrock geology; igneous rocks; volcanic rocks; felsic volcanic rocks; mafic volcanic rocks; volcaniclastics; sedimentary rocks; arenites; mudstones; conglomerates; structural features; deformation; gold; mineral deposits; iron formations; Woodburn Lake Group; Churchill Province; Precambrian
Illustrationssketch maps; photographs
Image
Released2003 06 01
AbstractThe Meadowbank gold project consists of five deposits hosted in the Neoarchean Woodburn Lake group of the western Churchill Province, including the recently delineated Vault deposit, located 7 km north-northeast of the previously defined mineralized zones in the 'Third Portage Lake' area. The supracrustal rocks of the Meadowbank area have experienced a polyphase deformation history spanning the Neoarchean to Paleoproterozoic. This contribution discusses the stratigraphic and structural framework of the corridor of rocks between the Meadowbank gold deposits and the recently discovered Vault deposit to the north.
GEOSCAN ID214396