File:Paradoxo11.jpg

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Português: Todas as amostras das ilhas havaianas que traçam em torno da linha inferior de referência (ΔNb = 0) são do estágio de formação do escudo de suas respectivas ilhas, enquanto aqueles que traçam ao redor da linha superior são do estágio de rejuvenescimento, conforme observado por. [29]
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Frey, F.A., Huang, S., Blichert-Toft, J., Regelous, M., and Boyet, M., 2005, Origin of depleted components in basalt related to the Hawaiian hot spot: Evidence from isotopic and incompatible element

ratios: Geochemistry, Geophysics, Geosystems, v. 6, art. no. Q02L07, doi: 10.1029/2004GC 000757
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Frey, F.A., Huang, S., Blichert-Toft, J., Regelous, M., and Boyet, M., 2005, Origin of depleted components in basalt related to the Hawaiian hot spot: Evidence from isotopic and incompatible element

ratios: Geochemistry, Geophysics, Geosystems, v. 6, art. no. Q02L07, doi: 10.1029/2004GC 000757

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current22:45, 12 August 2021Thumbnail for version as of 22:45, 12 August 20211,207 × 1,401 (401 KB)Rayanne.Bicalho (talk | contribs)Uploaded a work by Frey, F.A., Huang, S., Blichert-Toft, J., Regelous, M., and Boyet, M., 2005, Origin of depleted components in basalt related to the Hawaiian hot spot: Evidence from isotopic and incompatible element ratios: Geochemistry, Geophysics, Geosystems, v. 6, art. no. Q02L07, doi: 10.1029/2004GC 000757 from Frey, F.A., Huang, S., Blichert-Toft, J., Regelous, M., and Boyet, M., 2005, Origin of depleted components in basalt related to the Hawaiian hot spot: Evidence from isotopic and...

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