File:ParadoxoFigura10.jpg
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Português: A localização e composição dos montes submarinos dragados nos flancos da cordilheira East Pacific Rise(dados de Niu e Batiza, 1997). As duas linhas paralelas marcam os limites do arranjo da Islândia; O + representa a composição do manto primitivo. As montanhas submarinas variam em composição de basalto normal altamente empobrecido da dorsal meso-oceânica (N-MORB) para basalto alcalino enriquecido (Niu e Batiza, 1997) e se dividem em dois tipos de composição distintos de N-MORB (amarelo) e basalto de ilha
oceânica (OIB;vermelho) separados quase perfeitamente pela linha de referência ΔNb = 0.O histograma (codificado por cores quanto aos pontos de dados) mostra a distribuição bimodal fraca de ΔNb no conjunto de dados (oitenta amostras); a distribuição de Montes submarinos do tipo N-MORB e OIB são mostrados no mapa. Retirado de Fitton (2007). [20] |
| Date | |
| Source |
Fitton, J.G., 2007, The OIB paradox, in Foulger, G.R., and Jurdy, D.M., eds., Plates, plumes, and planetary processes: Geological Society of America Special Paper 430, p. 387–412, doi: 10.1130/2007.2430(20). |
| Author |
Fitton, J.G., 2007, The OIB paradox, in Foulger, G.R., and Jurdy, D.M., eds., Plates, plumes, and planetary processes: Geological Society of America Special Paper 430, p. 387–412, doi: 10.1130/2007.2430(20). |
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| current | 22:45, 12 August 2021 | | 1,439 × 872 (238 KB) | Rayanne.Bicalho (talk | contribs) | Uploaded a work by Fitton, J.G., 2007, The OIB paradox, in Foulger, G.R., and Jurdy, D.M., eds., Plates, plumes, and planetary processes: Geological Society of America Special Paper 430, p. 387–412, doi: 10.1130/2007.2430(20). from Fitton, J.G., 2007, The OIB paradox, in Foulger, G.R., and Jurdy, D.M., eds., Plates, plumes, and planetary processes: Geological Society of America Special Paper 430, p. 387–412, doi: 10.1130/2007.2430(20). with UploadWizard |
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