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Siberian craton mantle composition

Boyd F. R., Pokhilenko N. P., Pearson D. G., Mertzman S. A., Sobolev N. V., and Finger L. W. (1997) Composition of the Siberian cratonic mantle evidence from Udachnaya peridotite xenoliths. Contrib. Mineral. Petrol. 128, 228-246. [Pg.963]

Composition of the Siberian cratonic mantle evidence from Udachnaya peridotite xeno-liths. Contributions to Mineralogy and Petrology, 128, 228-246. [Pg.87]

Figure 18 Normative olivine and opx (garnet Uierzo-Ute norm) versus rock Mg showing low-T cratonic mantle relative to batch melt extraction trends from 3 GPa to 7 GPa (see Figure 6). Open circles are compositions from the Kaapvaal, Siberian, and Slave cratons, and the filled circles are compositions from the Tanzanian, Canadian, and Greenland cratons. Figure 18 Normative olivine and opx (garnet Uierzo-Ute norm) versus rock Mg showing low-T cratonic mantle relative to batch melt extraction trends from 3 GPa to 7 GPa (see Figure 6). Open circles are compositions from the Kaapvaal, Siberian, and Slave cratons, and the filled circles are compositions from the Tanzanian, Canadian, and Greenland cratons.
See other pages where Siberian craton mantle composition is mentioned: [Pg.1083]    [Pg.1084]    [Pg.1084]    [Pg.1085]    [Pg.1086]    [Pg.233]    [Pg.383]    [Pg.384]    [Pg.384]    [Pg.385]    [Pg.386]    [Pg.930]    [Pg.1085]    [Pg.66]    [Pg.67]    [Pg.228]    [Pg.385]   
See also in sourсe #XX -- [ Pg.383 , Pg.383 , Pg.384 , Pg.385 , Pg.386 ]



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