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


, : 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.


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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...

Chazot G.; Menzies M.A.; Harte B.; Mattey D., 1994: Carbonatite metasomatism and melting of the Arabian lithosphere; evidence from oxygen isotopes and trace element composition of spinel lherzolites. Mineralogical Magazine 58A(A-K): 167-168

Kempton P.D.; Hawkesworth C.J.; Lopez Escobar L.; Pearson D.G.; Ware A.J., 1999: Spinel+ or -garnet lherzolite xenoliths from Pali Aike; Part 2, Trace element and isotopic evidence bearing on the evolution of lithospheric mantle beneath southern Patagonia. Sr-Nd isotope compositions of Pali Aike xenoliths provide evidence for at least two episodes of depletion in the Pali Aike mantle, one ancient (Proterozoic?), the other more recent (Cenozoic). However, unusual concave-downward REE patterns are obs...

Kinzler R.J., 1994: Melting of mantle peridotite at pressures approaching the spinel to garnet transition. Mineralogical Magazine 58A(A-K): 483-484

Gaetani G.A.; Grove T.L., 1994: Melting in the sub-arc mantle; the effects of H (sub 2) O on primary magmas and the spinel-to-garnet transition. Mineralogical Magazine: A-K, Pages 301-302. 1994.

Sorokin A.A.; Drill S.I., 2000: The Yankan accretion complex as an example of spatial combination of OIB, BABB, N-MORB type metabasalts. International Geological Congress, Abstracts = Congres Geologique International, Resumes 31: (unpaginated

Kessel, R.; Ulmer, P.; Max, S.W.; Pettke, T., 2008: Experimental constraints on trace element partitioning during dehydration and melting of K-free MORB at 4-6 GPa and 700-1200 OC. Eos, Transactions, American Geophysical Union 89.53, Suppl.

Koga K.T.; Shimizu N.; Grove T.L., 1999: Disequilibrium trace element redistribution during garnet to spinel facies transformation. An experimental investigation has been made to examine trace element redistribution during garnet-spinel facies transformation that is characterized by the reaction, olivine + garnet --> clinopyroxene (cpx) + orthopyroxene (opx) + spinel, using...

Koga K.T., 1997: Kinetics of garnet to spinel facies transformation and trace element re-distribution. Eos, Transactions, American Geophysical Union: 6, Suppl., Pages 835. 1997.

Rosamond J.Kinzler, 1997: Melting of mantle peridotite at pressures approaching the spinel to garnet transition; application to mid-ocean ridge basalt petrogenesis. Journal of Geophysical Research: Solid Earth 102(B1): 853-874