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Detailed Reference Information |
Moreira, M., Kunz, J. and Allegre, C. (1998). Rare gas systematics in popping rock: Isotopic and elemental compositions in the upper mantle. Science 279(5354): 1,178-1,181. |
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New experimental data on the isotopic variations of neon, argon, and xenon in a popping rock imply that the Ar-40/Ar-36 ratio of the upper mantle is less than 44,000 and that the Xe-129/Xe-130 ratio is less than 8.2. The elemental abundance pattern of rare gases is chondritic-like and is quite distinct from the solar pattern. These data imply that Earth accreted from planetesimals that probably underwent a transformation of their rare gas budget from solar- to chondritic-like, leaving the isotopic composition unchanged from the solar pattern. |
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Abstract |
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Table 1 |
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Keywords
mid-atlantic ridge, noble-gases, ultramafic xenoliths, basalt glasses, neon, helium, evolution, xenon, 14-degrees-n, origin |
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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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