The influence of mantle metasomatism on the oxidation state of the lithospheric mantle
The oxidation state, reflected in the oxygen fugacity (fO2), of the lithospheric mantle is both laterally and vertically heterogeneous. Depth-fO2 profiles from kimberlite-borne peridotitic mantle xenoliths from the Bultfontein kimberlite, Kimberley, South Africa and the A154-N and A154-S kimberlites...
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| Format: | Others |
| Language: | en |
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2009
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| Online Access: | http://hdl.handle.net/10048/538 |