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Science 28 November 1997: Vol. 278. no. 5343, pp. 1595 - 1598 DOI: 10.1126/science.278.5343.1595
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Reports
Platinum-Group Element Abundance Patterns in Different Mantle Environments
Mark Rehkämper,
*
Alex N. Halliday,
Dan Barfod,
J. Godfrey Fitton,
J. Barry Dawson
Mantle-derived xenoliths from the Cameroon Line and northern
Tanzania display differences in their platinum-group element (PGE)
abundance patterns. The Cameroon Line lherzolites have uniform PGE
patterns indicating a homogeneous upper mantle over several hundreds of
kilometers, with approximately chondritic PGE ratios. The PGE patterns
of the Tanzanian peridotites are similar to the PGE systematics of
ultramafic rocks from ophiolites. The differences can be explained if
the northern Tanzanian lithosphere developed in a fluid-rich
suprasubduction zone environment, whereas the Cameroon Line lithosphere
only experienced melt extraction from anhydrous peridotites.
M. Rehkämper, A. N. Halliday, D. Barfod, Department of
Geological Sciences, University of Michigan, Ann Arbor, MI 48109-1063,
USA.
J. G. Fitton and J. B. Dawson, Department of Geology and Geophysics,
University of Edinburgh, Edinburgh EH9 3JW, UK.
*
To whom correspondence should be addressed. E-mail:
markrehk{at}umich.edu
Read the Full Text
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