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• W2065999153 abstract "Abstract Major element geochemistry, petrographic observations, and microprobe analyses of the Paleoproterozoic Serpent Formation, Huronian Supergroup, Canada, suggest that these strata experienced both potassium and sodium metasomatism. Major element data, plotted in Al2O3CaO∗ + Na2OK2O compositional space, form an array nearly identical to data from sub-Huronian paleosols reported elsewhere, suggesting that Serpent fluvial systems captured materials from entire weathering profiles. Potassium metasomatism was concentrated in shales, and represents the illitization of kaolinite, which is a residual product of plagioclase weathering. Sodium metasomatism principally affected silt- and sand-sized particles. Microprobe analyses of plagioclase grains indicate that they are nearly pure albite (>Ab96). Corresponding whole-rock major element data plot in bulk albite space on an (Al2O3K2O)CaO∗Na2O ternary diagram, whereas basement rocks plot in bulk andesine and oligoclase space. End member compositions and the absence of luminescence when bombarded with an electron beam indicate that the albites are of secondary origin. Extremely pure albite cements (>Ab99) commonly fringe detrital grains. There has been little replacement of detrital K-feldspars, despite the complete albitization of plagioclase grains. The timing of metasomatism, at least the last stage, is constrained to the period between ∼ 1700 and 1750 Ma (based on geochronologic data reported elsewhere), when the Southern Province of the Canadian Shield experienced considerable felsic plutonism, possibly related to arc collision. This plutonism may have resulted in the heating of deep basinal brines. Stresses associated with orogenic build-up, or gravity driven groundwater circulation working in concert with the plutonism, expelled these brines through the Serpent Formation (and the entire Huronian Supergroup), thoroughly metasomatizing the region. Such processes associated with collisional tectonics are akin to the development of Mississippi Valley-type PbZn mineralization in the mid-continent of the United States." @default.
• W2065999153 created "2016-06-24" @default.
• W2065999153 creator A5027329016 @default.
• W2065999153 date "1997-08-01" @default.
• W2065999153 modified "2023-09-25" @default.
• W2065999153 title "Potassic and sodic metasomatism in the Southern Province of the Canadian Shield: Evidence from the Paleoproterozoic Serpent Formation, Huronian Supergroup, Canada" @default.
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• W2065999153 cites W2040236851 @default.
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• W2065999153 cites W2503995335 @default.
• W2065999153 cites W2908651752 @default.
• W2065999153 cites W2908854015 @default.
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• W2065999153 doi "https://doi.org/10.1016/s0301-9268(96)00058-7" @default.
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