Remobilization in the Cratonic Lithosphere Recorded in Polycrystalline Diamond
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. Framesites are defined as polycrystalline aggregates of diamond with crystals smaller than 1 mm.
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CaO contents in eclogitic garnets from framesites range between 2.70 and 8.18 wt % with an average of 4.73 wt % (24); those of garnets in eclogite xenoliths average 6.84 wt % ( n = 182) and range between 3.3 and 21.69 wt % (25 26).
Mg number = MgMg+Fe×100.
. These authors report a negative correlation for δ 13 C and wt % FeO in olivines from southern African peridotitic diamond inclusions.
T. E. McCandless et al. paper presented at the 28th International Geological Congress Washington DC 1989.
Subcalcic garnets are harzburgitic (depleted) minerals with low CaO contents (<2 wt %) but high Cr 2 O 3 contents (up to 18 wt %) (27). Typically they have LREE-enriched trace element signatures and unradiogenic ε Nd(i) values down to −60 ε (28). Sm/Nd ratios are 0.02 to 0.80 (29).
All grains used for either isotope measurements or LAM were fresh and optically clear up to a magnification of 500 and were thoroughly acid leached after hand-picking (30) followed by optical rechecks. Inclusions of other minerals such as carbonate or apatite would also be evident from abrupt changes in the time-resolved signal for Ca and Si.
1 × 10 −18 cm/s 2 : R. Coghlan thesis Brown University Providence RI (1990).
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K. S. Viljoen unpublished data.
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P. Cartigny thesis Université Paris 7 (1997).
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. Trace element data are available at www.sciencemag.org/feature/data.1051804.shl.
This study was supported by Deutsche Forschungsgemeinschaft grants Ja 781/2-1 and Ja 781/2-2 to D.J. We thank D. Mattey for providing access to his efficient stable isotope lab and P. Cartigny for measuring the carbon isotopes. Framesite samples were provided by DeBeers. We thank three anonymous reviewers for constructive criticism.