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- W1984179600 abstract "The lavas of the Cameroon line display a lead isotope anomaly at the continent/ocean boundary which can be attributed to a fossil mantle plume, the diminishing lateral effects of which can be recognized as far as 400km to either side. The high 206Pb/204Pb ratio—characteristic of the mantle endmember known as 'HIMU'—seems to arise from U/Pb fractionation accompanying melt migration following emplacement of the plume in the upper mantle 125 Myr ago." @default.
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- W1984179600 date "1990-10-01" @default.
- W1984179600 modified "2023-10-18" @default.
- W1984179600 title "Trace-element fractionation in plumes and the origin of HIMU mantle beneath the Cameroon line" @default.
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- W1984179600 doi "https://doi.org/10.1038/347523a0" @default.
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