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Trace elements

Trace elements. Chapter 2. Why use trace elements?. Note magnitude of major element changes.

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Mantle Convection

Mantle Convection. Geochemical Reservoirs . Primitive mantle composition Is inferred from chondrites Continental crust, EM1, HIMU enriched in incompatibles; MORB depleted MORB shows inverse pattern from Cont. Crust suggesting crust forms by extraction from MORB

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Rb incompatible - PowerPoint PPT Presentation

Trace elements

Mantle Convection