Subcontinental versus suboceanic mantle, II. Nd-Sr-Pb isotopic comparison of continental tholeiites with mid-ocean ridge tholeiites, and the structure of the continental lithosphere

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Scientific paper

Nd-Sr-Pb isotopic measurements for continental flood basalts from the Deccan traps and dolerites from Tasmania show that variations in these basalts are related to continental crust contamination in agreement with Faure et al.'s [3] conjecture for Antarctic basalts. The source of these basalts have peculiar depleted characters and it is proposed that such a source is the layered continental lithosphere.

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