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- W2015168498 abstract "Abstract Braunite occurs in shales in the Proterozoic Manganese Group, Western Australia as flattened concretions which post-date the shale sedimentation and pre-date lithification. The mineral is here classified as diagenetic in origin. Braunite may have grown as concretions in the still-most sediment by reaction between Mn 2+ , liberated from older manganese oxides by decay of trapped organic remains, and silica. Apatite within the nodules possibly results from organically-derived phosphate. Polycrystalline braunite also occurs in the Manganese Group sediments, as a result of recrystallisation of an older generation of braunite of undefined genesis." @default.
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- W2015168498 modified "2023-09-27" @default.
- W2015168498 title "Diagenetic braunite in sedimentary rocks of the proterozoic Manganese Group, Western Australia" @default.
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- W2015168498 doi "https://doi.org/10.1016/0169-1368(90)90036-m" @default.
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