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

Gleeson, S. A.; Turner, W. A.

doi:10.1111/j.1468-8123.2006.00160.x

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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

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Gleeson, S. A.
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Turner, W. A.
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Gleeson, S. A., Turner, W. A. (2007): 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. - Geofluids, 7, 1, 51-68.
https://doi.org/10.1111/j.1468-8123.2006.00160.x

Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_1943891

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 'Presqu'ile' dolomite that preferentially replaced some of the upper barrier limestones. The main ore-stage sulfides include galena, sphalerite, marcasite, and pyrite. A bulk fluid inclusion chemistry study was carried out on sulfide, coarse non-saddle and saddle dolomite and calcite samples from the Pine Point and Great Slave Reef deposits, and unmineralized coarse non-saddle and saddle dolomite samples from Hay West, Windy Point and Qito areas. Molar Cl/Br ratio data from Pine Point indicate the presence of four fluids at different stages of the paragenesis. The fluids trapped in sulfides and ore-stage dolomites predominately consist of a Br-rich fluid with a composition similar to that of evaporated seawater (fluid A), and a very Br-enriched fluid of unknown origin (fluid B). Both these fluids are CaCl2-NaCl (Na to Ca ratios of 1:10)-rich brines and have compositions unlike the modern formation waters in the Devonian aquifers in the basin today. A third, relatively Cl-rich (or Br-poor), fluid (fluid C) was identified in two samples and may have acquired some chlorinity by dissolving halide minerals. Mixing between the Br-rich fluid A and a dilute fluid also occurred in the later stages of the paragenesis, resulting in the formation of calcite and native sulfur. Saddle and coarse dolomites not associated with significant sulfide mineralization have a narrow range of halogen compositions similar to fluid A. There is no evidence of fluid B or C in the unmineralized samples. Relative to a modern-day seawater compositions all the fluids have had some modification of their cation compositions. There is some weak evidence for interactions with clastic units or crystalline basement rocks. It is also possible however, that the evaporative brines could have formed from a relatively CaCl2-rich, NaCl-depleted Devonian seawater, unlike the composition of modern-day seawater.