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- W2156321503 abstract "Continental flood basalts and mid‐ocean ridge (MOR) tholeiitic basalts have distinctly different 143 Nd/ 144 Nd which may permit a priori distinction between continental and oceanic igneous rocks. Initial 143 Nd/ 144 Nd of continental igneous rocks through time fall on a Sm/Nd evolution curve with chondritic REE abundance ratio. These observations indicate that many continental igneous rocks are derived from a reservoir with chondritic REE pattern which may represent primary material remaining since the formation of the earth. Oceanic igneous rocks are derived from a different ancient reservoir which has Sm/Nd higher than chondritic. Initial 143 Nd/ 144 Nd and 87 Sr/ 86 Sr in young basalts from both oceans and continents show a strong correlation suggesting that Sm‐Nd and Rb‐Sr fractionation events in the mantle may be correlative and caused by the same process. From this correlation Rb/Sr for the earth is inferred to be 0.029." @default.
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- W2156321503 date "1976-12-01" @default.
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- W2156321503 title "Inferences about magma sources and mantle structure from variations of<sup>143</sup>Nd/<sup>144</sup>Nd" @default.
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- W2156321503 doi "https://doi.org/10.1029/gl003i012p00743" @default.
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