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Science 15 September 1995: Vol. 269. no. 5230, pp. 1535 - 1540 DOI: 10.1126/science.7667634
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Articles
Science, Vol 269, Issue 5230, 1535-1540
Copyright © 1995 by American Association for the Advancement of Science
The Earth's early evolution
SA Bowring
and
T Housh
Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge 02139, USA.
The Archean crust contains direct geochemical information of the Earth's early planetary differentiation. A major outstanding question in the Earth sciences is whether the volume of continental crust today represents nearly all that formed over Earth's history or whether its rates of creation and destruction have been approximately balanced since the Archean. Analysis of neodymium isotopic data from the oldest remnants of Archean crust suggests that crustal recycling is important and that preserved continental crust comprises fragments of crust that escaped recycling. Furthermore, the data suggest that the isotopic evolution of Earth's mantle reflects progressive eradication of primordial heterogeneities related to early differentiation.
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