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- W2013533842 abstract "In the pre-3.7 Ga old Isua supracrustal belt, West Greenland, a banded iron-formation occurs. The iron-formation can be subdivided into different facies according to composition and mineralogy, and these facies resemble the facies subdivision of younger Archaean and Precambrian iron-formations. The geochemistry of the Isua iron-formation indicates that the secular variation in the contents of phosphorus, calcium and aluminium as well as the Na/K ratios of Precambrian iron-formations can be extended into the Early Archaean. A remarkable feature of the Isua iron-formation is the high chalcopyrite/iron-sulphide ratio. Field relationships and geochemical evidence indicate that the iron-formation is mainly of submarine-exhalative origin from brines of basaltic pedigree." @default.
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- W2013533842 date "1980-02-01" @default.
- W2013533842 modified "2023-09-27" @default.
- W2013533842 title "On the early archaean isua iron-formation, West Greenland" @default.
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- W2013533842 doi "https://doi.org/10.1016/0301-9268(80)90081-9" @default.
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