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- W2010479568 abstract "High-temperature deformed garnet lherzolite xenoliths from mantle beneath the northern Lesotho margin of the Archaean craton in southern Africa are inferred to have been in internal Nd and Sr isotopic equilibrium at the time of sampling by kimberlite 90 Ma ago. Their trace element and isotopic signatures resemble those of depleted (high Sm/Nd, low Rb/Sr) MORB-type mantle from the convective asthenosphere. The common lower-temperature coarse and deformed garnet lherzolite xenoliths from beneath the Kimberley area in the craton interior display internal isotopic equilibrium or, alternatively, inverse isotopic disequilibrium attributable to recent mantle metasomatic component addition or redistribution. These lherzolites bear trace element and isotopic signatures of variously enriched (low Sm/Nd, high Rb/Sr) mantle stabilized in subcontinental lithosphere for up to 3 Ga. As a group the lithospheric peridotites provide an extreme range of isotopic compositions for potential contamination of continental volcanics." @default.
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- W2010479568 date "1985-10-01" @default.
- W2010479568 modified "2023-10-14" @default.
- W2010479568 title "Kimberlite-borne garnet peridotite xenoliths from old enriched subcontinental lithosphere" @default.
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- W2010479568 doi "https://doi.org/10.1016/0012-821x(85)90094-9" @default.
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