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- W1008173325 abstract "This chapter discusses the chemical factors in the deposition and diagenesis of banded iron-formation (BIF). The chapter attempts to bring together chemical factors involved in the supply of constituents and in the processes of deposition, segregation, consolidation, and alteration that have produced these remarkable rocks. It is concerned, therefore, with both quantity and concentration, with equilibrium and non-equilibrium, and with processes both in solution and in the primary sediments. The most comprehensive account of the chemical aspects of this topic is the monograph by Mel’nik. Even in fresh and relatively unmetamorphosed rocks, there are marked variations in composition with the four end-member facies, oxide, silicate, carbonate and sulfide, and many mixed facies. There are also variations that are derived from depositional environment, from the shallowwater oolitic, and granular forms to the deeper-water finely banded rocks, which appear to have escaped the effects of wave or current turbulence. It is these finely banded rocks that might be expected to retain the most information concerning the detailed sequence of deposition, a view that is reinforced by the extraordinary lateral continuity of the fine banding in some of them." @default.
- W1008173325 created "2016-06-24" @default.
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- W1008173325 date "1983-01-01" @default.
- W1008173325 modified "2023-10-10" @default.
- W1008173325 title "Chapter 13 Chemical Factors in the Deposition and Diagenesis of Banded Iron-Formation" @default.
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- W1008173325 doi "https://doi.org/10.1016/s0166-2635(08)70054-9" @default.
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