Is eclogite in the sub-continental lithosphere the residue from melting of subducted oceanic crust? Experimental constraints and implications for the origin of the Archean continents

Most read articles by the same author(s)

• R.P. Rapp, S. Timmerman, J. Lowczak, A.L. Jaques, Metasomatism of cratonic lithosphere by hydrous, silica-rich, fluids derived from recycled sediment: experimental insights at 5-7 GPa , International Kimberlite Conference: Extended Abstracts: Vol. 11 (2017): Vol 11: International Kimberlite Conference, Gaborone
• S.F. Foley, G.M. Yaxley, R.P. Rapp, D.E. Jacob, Experimental melting of peridotites in the presence of CO2 and H2O at 40-60 kbar , International Kimberlite Conference: Extended Abstracts: Vol. 9 (2008): Vol 9: International Kimberlite Conference, Frankfurt
• R.P. Rapp, N. Shimizu, On the origin of eclogite and websterite parageneses in the cratonic mantle, and their relationship to TTG granitoid magmatism , International Kimberlite Conference: Extended Abstracts: Vol. 8 (2003): Vol 8: International Kimberlite Conference, Victoria
• R.P. Rapp, N. Shimizu, Subduction and slab melting in the Archean: experimental constraints and implications for development of cratonic lithosphere , International Kimberlite Conference: Extended Abstracts: Vol. 7 (1998): Vol 7: International Kimberlite Conference, Cape Town
• R.P. Rapp, G.M. Yaxley, M.D. Norman, Continent formation in the Archean and chemical evolution of the cratonic lithosphere , International Kimberlite Conference: Extended Abstracts: Vol. 9 (2008): Vol 9: International Kimberlite Conference, Frankfurt