Geochronological constraints on the genesis of high-grade iron ore in the Gongchangling BIFs from the Anshan-Benxi area, North China Craton

Ore Geology Reviews(2020)

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摘要
•The garnet was formed during prograde metamorphism by trace element.•The metamorphic age was 1888 ± 77 Ma by garnet Sm-Nd isochron.•The metamorphic hydrothermal fluid reformed BIFs to produce high-grade iron ore.
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关键词
Gongchangling,Algoma-type BIFs,High-grade iron ore genesis,North China Craton,Zircon U–Pb geochronology,Garnet Sm–Nd isochron
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