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From a study of first-transition series trace elements and low-partition-coefficient trace elements or so-called hygromagmatophyle elements (Treuil and Varet, 1973; Treuil and Joron, 1976), we will try to define the relative importance of the three fundamental parametersmantle source composition, extent of partial melting, and crystal fractionation—which bear on the formation of basalts recovered during Leg 45. We relate the presented data to the results of shipboard study (Chapters 7 and 8, this volume) and then give a tentative interpretation, taking into account our present knowledge of the behavior of trace elements during magmatic processes of FAMOUS and Leg 37 results.

Trace Elements in Basalts from 23°N and 36°N in the Atlantic Ocean: Fractional Crystallization, Partial Melting, and Heterogeneity of the Upper Mantle