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• W1647501350 abstract "Publisher Summary This chapter discusses the occurrence, geologic associations, age distributions, physical and chemical properties, probable origin, and mineralogic evolution of Precambrian iron-formations. The Precambrian iron-formations are quantitatively relatively minor components in the Precambrian sedimentary record. However, in addition to their great economic value, they are significant indicators of certain large-scale aspects of the earth's evolution. Iron-formation exposed in the earth's crust today is the product of a sequence of processes that involved initial sedimentation, diagenesis, and one or more epochs of metamorphism. Each of these stages left its imprint on the rock, texturally or mineralogically. The nature of iron-rich accumulates is governed to a large degree by the prevailing environment. The processes involved in diagenesis of iron-formation, include dewatering and compaction, dehydration and crystallization of gels, biochemical reduction of dissolved sulfate to yield reactive H 2 S, and mineralogic reactions in response to the physicochemistry of the burial environment. At the other end of the metamorphic spectrum are the coarsely crystalline iron-formations in contact with large mafic intrusions, such as the Duluth Gabbro and the Stillwater Complex, and the products of high-grade regional metamorphism, as in the Archean-age ironformation of the Yilgarn Block of Western Australia." @default.
• W1647501350 created "2016-06-24" @default.
• W1647501350 creator A5007316792 @default.
• W1647501350 date "1992-01-01" @default.
• W1647501350 modified "2023-09-30" @default.
• W1647501350 title "Chapter 11 Precambrian Iron-Formations: Nature, Origin, and Mineralogic Evolution from Sedimentation to Metamorphism" @default.
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• W1647501350 doi "https://doi.org/10.1016/s0070-4571(08)70573-9" @default.
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