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Iron ends up in sedimentary rock primarily through the weathering and erosion of igneous and metamorphic rocks that contain iron minerals. As these rocks break down, iron can be transported by water, wind, or ice into sedimentary environments, where it may precipitate or be incorporated into sediments. Over time, these sediments accumulate, and through processes like compaction and cementation, they form sedimentary rock that may contain iron in various forms, such as iron oxides or iron-bearing minerals.

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1mo ago

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