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- W4224059937 abstract "Xuanlong ironstones occur as stromatolitic or ooidal, hematite-rich, concordant bodies in the Paleoproterozoic Chuanlinggou Formation of North China. Continental-derived iron was traditionally suggested as the ironstone source. However, widespread hydrothermal discharge chimney structures have been discovered. These structures are interpreted as fluid-flow pathways resulting from the ejection of hydrothermal fluids into unconsolidated sandy sediments in a shallow subtidal zone. Simple tubular and curviplanar structures outlined by the occurrence of Fe-rich silicified sediments are well-developed in the underlying sandstones. Honeycomb-like cavities and possible fluid-flow channel textures attest to primary porosity during the formation of the ironstones, indicating that hydrothermal fluids play a key role in the formation of ironstones. This study provides an unequivocal example of Paleoproterozoic shallow-water hydrothermal activity for the first time, which is of great significance in understanding the genesis of granular or Superior-type IFs in general." @default.
- W4224059937 created "2022-04-19" @default.
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- W4224059937 date "2022-07-01" @default.
- W4224059937 modified "2023-10-02" @default.
- W4224059937 title "Shallow-water hydrothermal venting and the formation of Precambrian ironstones: Insights from the terminal-Paleoproterozoic Xuanlong ironstones in North China Craton" @default.
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- W4224059937 doi "https://doi.org/10.1016/j.precamres.2022.106667" @default.
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