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Strontium primitive mantle composition

In the early days of mantle geochemistry, the composition of the bulk silicate earth, also called primitive mantle (i.e., mantle prior to the formation of any crust see Chapter 2.01) was not known for strontium isotopes because of the obvious depletion of rubidium of the Earth relative to chondritic meteorites (Gast, 1960). [Pg.798]


See other pages where Strontium primitive mantle composition is mentioned: [Pg.1210]    [Pg.1212]    [Pg.512]    [Pg.514]    [Pg.930]    [Pg.1204]    [Pg.1617]    [Pg.228]    [Pg.506]    [Pg.286]   
See also in sourсe #XX -- [ Pg.14 ]




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