Fluid inclusion constraints on the origin of the brines responsible for Pb–Zn mineralization at Pine Point and coarse non‐saddle and saddle dolomite formation in southern Northwest Territories

• Published in: Geofluids
• Main Authors: GLEESON, S. A., TURNER, W. A.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2006
• Subjects: Northwest Territories
• Online Access: http://dx.doi.org/10.1111/j.1468-8123.2006.00160.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1468-8123.2006.00160.x; https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1468-8123.2006.00160.x

Abstract The Pine Point region is a classic metallogenic mining camp that produced over 58 million short tons of Zn–Pb ore from approximately 40 base‐metal mineralized deposits hosted by Middle Devonian carbonates. The ore deposits are localized in paleokarstic features found in the epigenetic ‘Pres...