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Stephen H. Richardson

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Created 2026-10-25 Updated 2026-11-05  0 By others on same topic  0 Discussions Create my own version
Stephen H. Richardson and Steven B. Shirey used chemical and isotopic information from diamond inclusions to investigate recycling into ancient lithospheric mantle. A change in inclusion assemblages motivated a proposed connection with subduction and continental collision.[ref]
The inclusions preserve deep material, but their ages and origin must be related carefully to diamond growth and later transport.
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  • Start of the Wilson cycle at 3 Ga shown by diamonds from subcontinental mantle by Steven B. Shirey and Stephen H. Richardson

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