NB AND PB IN OCEANIC BASALTS: NEW CONSTRAINTS ON MANTLE EVOLUTION
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NB AND PB IN OCEANIC BASALTS: NEW CONSTRAINTS ON MANTLE EVOLUTION
Hofmann A.W.; Jochum K.P.; Seufert M.; White W.M.
xmlui.dri2xhtml.METS-1.0.item-citation:
EARTH AND PLANETARY SCIENCE LETTERS, 1986, 79, 1-2, 33-45
Date:
1986
Abstract:
Nb/U ratios and Ce/Pb ratios are surprisingly uniform at 47 _+ 10 and 25 ___ 5, respectively, in both mid-ocean ridge
basalts (MORB) and ocean island basalts (OIB). We show that these ratios also characterize the mantle sources of both
types of oceanic basalts, and that these mantle sources have been fractionated from the primitive-mantle ratios of
Nb/U = 30 and Ce/Pb = 9. The respective ratios in the continental crust are even lower, namely Nb/U = 10 and
Ce/Pb = 4. Therefore, OIB cannot be derived from a primitive portion of the mantle, from mixtures of primitive and
depleted mantle, or from recycled continental crust. The portion of the primitive mantle from which the continental
crust and the residual (MORB plus OIB source) mantle has been differentiated is estimated to be about 50%, but the
uncertainties are such that whole-mantle differentiation cannot be ruled out.
We propose the following simple model to satisfy the above new constraint on mantle composition: The differenti-
ated part of the mantle, chemically depleted after separation of the major portion of the continental crust, was
subsequently internally rehomogenized. This depleted but chemically homogeneous mantle region was then differenti-
ated into MORB and OIB source regions. The primary (continental crust-mantle) differentiation fractionated the
Nb/U and Ce/Pb ratios, but the secondary (MORB source-OIB source) differentiation did not. Following the model
of Hofmann and White [1,2], we suggest that the mechanism chiefly responsible for the secondary differentiation is the
formation and subduction of oceanic crust. It is volumetrically by far the most important ongoing differentiation
process on Earth and, over the course of Earth history, has created at least ten times as much oceanic crust as the
present-day volume of continental crust.
Because the residual mantle was homogenized (though depleted in incompatible elements) after the primary
differentiation, the isotopic and chemical heterogeneities exemplified by the isotope ratios of Sr, Nd, Hf, and Pb, and
by trace element ratios such as K/Rb, were created during the secondary differentiation. During this process, the bulk
partition coefficients of Nb and Ce were very similar to those of U and Pb, respectively. This is in contrast with the
primary differentiation, during which U was more incompatible than Nb, and Pb more incompatible than Ce.
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