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Udachnaya kimberlite

Snyder G. A., Jerde E. A., Taylor L. A., Halliday A. N., Sobolev V. N., and Sobolev N. V. (1993) Nd and Sr isotopes from diamondiferous eclogites, Udachnaya kimberlite pipe, Yakutia, Siberia evidence of differentiation in the early Earth Earth. Planet. Sci. Lett. 118, 91-100. [Pg.975]

Shatsky V. S., Sobolev N. V., and Pavlyuchenko V. S. (1983) Fassaite-garnet-anorthite xenolith from the Udachnaya kimberlite pipe, Yakutia. Dokl. Akad. Nauk. SSSR 272(1), 188-192. [Pg.1328]

Fig. 3. Trd ages of Siberian whole-rock peridotites (Pearson et al. 1995ft), mostly from the Udachnaya kimberlite, compared with Tma ages of sulphides from Udachnaya olivine macrocrysts (Pearson et al. 2000) and Tma ages from Udachnaya diamond inclusions (Pearson et al. 1999). Fig. 3. Trd ages of Siberian whole-rock peridotites (Pearson et al. 1995ft), mostly from the Udachnaya kimberlite, compared with Tma ages of sulphides from Udachnaya olivine macrocrysts (Pearson et al. 2000) and Tma ages from Udachnaya diamond inclusions (Pearson et al. 1999).
A diamond bearing kimberlite pipe was discovered in Siberia in 1954. There are at least 300 kimberlite pipes in Siberia. The most productive of these is the Udachnaya mine near the town of Udachnaya. [Pg.685]


See other pages where Udachnaya kimberlite is mentioned: [Pg.929]    [Pg.946]    [Pg.948]    [Pg.1040]    [Pg.1302]    [Pg.70]    [Pg.227]    [Pg.244]    [Pg.246]    [Pg.339]    [Pg.929]    [Pg.946]    [Pg.948]    [Pg.1040]    [Pg.1302]    [Pg.70]    [Pg.227]    [Pg.244]    [Pg.246]    [Pg.339]    [Pg.939]    [Pg.946]    [Pg.948]    [Pg.949]    [Pg.237]    [Pg.244]    [Pg.246]    [Pg.247]   
See also in sourсe #XX -- [ Pg.70 ]




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