Article ID Journal Published Year Pages File Type
6442255 Precambrian Research 2015 16 Pages PDF
Abstract

- The Nanfen iron deposit belongs to Algoma type BIF.
- The formation age of the Nanfen deposit is constrained at 2552 Ma.
- The high-grade ores formed by metamorphic hydrothermalism at 2482 Ma.
- The Nanfen deposit was benefited from ∼2.55 Ga crustal growth processes.
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Preview
Geochronology and geochemistry of the Nanfen iron deposit in the Anshan-Benxi area, North China Craton: Implications for ∼2.55 Ga crustal growth and the genesis of high-grade iron ores
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