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E-MORB- and OIB-type metabasalts from the Karakaya Complex; trace element evidence from melting across the spinel-garnet transition






Eos, Transactions, American Geophysical Union 89.53, Suppl.

E-MORB- and OIB-type metabasalts from the Karakaya Complex; trace element evidence from melting across the spinel-garnet transition



Accession: 037038290



Related references

Reiners Peter W., 1997: Kinetic inhibition of the garnet-spinel phase transition in upwelling mantle peridotite beneath mid-ocean ridges; a plausible but unlikely explanation for MORB garnet-signature. Trace element and isotopic evidence unambiguously indicate that garnet is residual in the source of nearly all mid-ocean ridge basalts (MORB), and that the extent of melting in the presence of residual garnet is inversely correlated with total ext...

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