Iron deposits hosted by banded iron-formations in the Yilgarn Craton: Products of sequential iron enrichment by magmatic, marine and meteoric fluids
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DOI: 10.1016/j.oregeorev.2019.103251
Abstract: Abstract Mesoarchean Algoma-type BIF in the Yilgarn Craton are locally enriched by secondary processes to iron concentrations approaching 72 wt% Fe. While their near-surface goethite–hematite ores are unequivocally the product of supergene fluid alteration, their… read more here.
Keywords: deposits hosted; bif; iron deposits; yilgarn craton ... See more keywords