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• W2023168625 endingPage "451" @default.
• W2023168625 startingPage "443" @default.
• W2023168625 abstract "Helium, neon, and argon isotopic compositions were measured in two flows of the Columbia River flood basalt. The Imnaha Basalt has a 3He/4He ratio of 11.4 times atmospheric and 20Ne/22Ne and 21Ne/22Ne ratios characteristic of a plume component. The measured 3He/4He is a lower limit, due to possible preferential 3He loss and/or addition of radiogenic 4He. A Wanapum Basalt flow, erupted approximately 2 Ma later in the waning stages of volcanism, has more MORB-like noble gases. The He, Nd and Sr isotopic compositions of these lavas suggest that the Columbia River basalts were derived from the Yellowstone plume head which contained both ‘high-helium’ plume material and entrained depleted mantle. As the eruptions progressed the plume component in the melting region was gradually diluted or replaced." @default.
• W2023168625 created "2016-06-24" @default.
• W2023168625 creator A5019076356 @default.
• W2023168625 creator A5035484376 @default.
• W2023168625 creator A5044343097 @default.
• W2023168625 date "1997-08-01" @default.
• W2023168625 modified "2023-10-17" @default.
• W2023168625 title "Helium and neon isotopes in the Imnaha Basalt, Columbia River Basalt Group: Evidence for a Yellowstone plume source" @default.
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• W2023168625 doi "https://doi.org/10.1016/s0012-821x(97)00090-3" @default.
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