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Osmium mantle geochemistry

U and U, and this is in part responsible for the more complex isotopic relationships displayed by lead isotopes in comparison with the systematics of strontium, neodymium, hafnium, and osmium isotopes. The mantle geochemistry of noble gases, although of course an integral part of mantle geochemistry, is treated in Chapter 2.06. [Pg.773]

Hanghoj, K., Keleman, P. B., Bernstein, S., Blustz-TAJN, J. Frei, R. 2001. Osmium isotopes in the Weidemann Fjord mantle xenoliths, a unique record of cratonic mantle formation by melt depletion in the Archean. Geochemistry, Geophysics and Geosystems, 2, 85-92. [Pg.87]

See other pages where Osmium mantle geochemistry is mentioned: [Pg.769]    [Pg.66]    [Pg.768]    [Pg.778]    [Pg.907]    [Pg.1201]    [Pg.3404]    [Pg.65]    [Pg.75]    [Pg.205]    [Pg.503]   
See also in sourсe #XX -- [ Pg.75 , Pg.76 ]



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