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Carbon elemental and isotopic composition in mantle xenoliths from Spain: Insights on sources and petrogenetic processes
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文摘
Carbon elemental and isotopic composition of mantle xenoliths from Iberian Peninsula C-δ13C suggests juvenile carbon origin and Rayleigh-type fractionation. δ13C-87Sr/86Sr correlation indicates metasomatic components. Evidence of carbon recycling via subduction in the mantle beneath Betic Cordillera

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