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• W2046342287 endingPage "107" @default.
• W2046342287 startingPage "95" @default.
• W2046342287 abstract "The alteration of detrital biotites has been studied in two clastic Proterozoic sedimentary sequences from southern and central Sweden, namely the Visingsö Group and the Dala Sandstone, respectively. The results showed that the biotites are altered through replacement by clay minerals (illite, chlorite and less commonly kaolinite). Biotite may either be replaced pseudomorphically (one biotite crystal by one clay mineral crystal) or by fine-crystalline clay minerals which merge into the interstitial clay matrix. In reddish rocks, biotite may be associated with pigmentary hematite and in greenish rocks with pyrite. The variation in the two textural habits of biotite alteration, i.e., pseudomorphic or fine crystalline, is related to physico-chemical properties of pore solution and nature of biotite particles." @default.
• W2046342287 created "2016-06-24" @default.
• W2046342287 creator A5057027693 @default.
• W2046342287 creator A5079044891 @default.
• W2046342287 date "1986-04-01" @default.
• W2046342287 modified "2023-09-23" @default.
• W2046342287 title "Diagenetic alteration of detrital biotite in Proterozoic sedimentary rocks from Sweden" @default.
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• W2046342287 doi "https://doi.org/10.1016/0037-0738(86)90073-4" @default.
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