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Thermochemical regime of the early mantle inferred from numerical models of the coupled magmatism-mantle convection system with the solid-solid phase transitions at depths around 660 km



Thermochemical regime of the early mantle inferred from numerical models of the coupled magmatism-mantle convection system with the solid-solid phase transitions at depths around 660 km



Journal of Geophysical Research: Solid Earth 103(B6): 12161-12180




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Accession: 020483487

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DOI: 10.1029/98jb00611


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