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I 200km Lithosphere . ,vapor, ,' ':•-.. framework and a dynamic model are probably smaller than those involved in the uncertainties • about the variation of oxygen fugacity in the mantle and its effect on solidus temperatures. Figures 6 and 7 are therefore suitable for illustrating the types of reactions and processes to be expected in a plume reaching the lithosphere. If there are volatile components in the deep • cm 100 Trace ofmelt•••-• 150 C-H-Ovapor • 200 100 mantle, H20 is released from the hydrates as the plume molten source became permeable.

Volcanic and chemical evolution of the Canary Islands, in Geology of the Northwest African Margin, edited by U. , pp. 273-306, Springer-Verlag, New York, 1982. , A petrologic model for the constitution of the upper mantle and crust of the Koolau shield, Oahu, Hawaii, and Hawaiian magmatism, Earth Planet. Sci. , 62, 215-228, 1983. Sinha, M. , K. E. Louden, and B. J. R. Astron. , 66, 351-377, 1981. H. Sleep, Some simple physical models for absoluteplate motions,J. , 79, 2557-2567, 1974. Sparks, R.

Peck, and H. R. Monogr. , vol. 19, edited by G. H. Sutton, M. H. Manghnani, and R. Moberly, pp. , 1976. Zucca, J. , and D. P. Hill, Crustal structure of the southeast flank of the Kilauea volcano, Hawaii, from seismic refraction measurements, Bull. Soc. , 70, 1149-1159, 1980. Zucca, J. , D. P. Hill, and R. L. Kovach, Crustal structure of Mauna Loa volcano,Hawaii, from seismicrefractionand gravity data, Bull. Soc. , 72, 1535-1550, 1982. 6004, 1978. Watts, A. , and J. R. Cochran, Gravity anomalies and flexure of the T.

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