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Detailed Reference Information |
Blichert-Toft, J., Frey, F.A. and Albarede, F. (1999). Hf isotope evidence for pelagic sediments in the source of Hawaiian basalts. Science 285(5429): 879-882. |
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Lead, oxygen, and osmium isotopic ratios measured on Hawaiian basalts can be matched with the isotopic ratios inferred for recycled ancient oceanic crust. High-precision hafnium isotopic data for lavas from several Hawaiian volcanoes identify old pelagic sediments in their source. These observations support the recycling hypothesis, whereby the mantle source of ocean island basalts includes ancient subducted oceanic crust. Hyperbolic lead-hafnium isotopic relations among Hawaiian basalts further indicate that upper mantle material is not involved in the production of hot spot basalts. |
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BACKGROUND DATA FILES |
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Abstract |
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Table 1 |
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Keywords
oceanic basalts, ferromanganese nodules, haleakala volcano, marine-sediments, mantle evolution, crust, constraints, geochemistry, lavas, seawater |
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Publisher
American Association for the Advancement of Science 1200 New York Avenue NW Washington, DC 20005 1-202-326-6540 1-202-682-0816 webmaster@aaas.org |
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