1. Agashev, A.M., Orikhashi Yu., Watanabe, T., et al., Isotope- geochemical characteristics of kimberlites of the Siberian Platform in relation with problem of their origin, Geol. Geofiz., 2000, vol. 41, no. 1, pp. 90–99.
2. Ashchepkov, I.V., Pokhilenko, N.P., Vladykin, N.V., et al., Tectonophysics structure and evolution of the lithospheric mantle beneath Siberian Craton, thermobarometric study, Tectonophysics, 2010, vol. 485, nos. 1–4, pp. 17–41.
3. Ashchepkov, I.V., Vladykin, N.N., Ntaflos, T., et al., Layering of the lithospheric mantle beneath the Siberian Craton: modeling using thermobarometry of mantle xenolith and xenocrysts, Tectonophysics, 2014, vol. 634, pp. 55–75.
4. Ashchepkov, I.V., Kuligin, S.S., Vladykin, N.V., et al., Comparison of mantle lithosphere beneath Early Triassic kimberlite fields in Siberian Craton reconstructed from deep-seated xenocrysts, Geosci. Front., 2015, doi 10.1016/j.gsf.2015.06.004
5. Atlas-opredelitel’ porod i rud mestorozhdenii almazov kimberlitovogo tipa (Identificatiom Atlas of Rocks and Ores of the Kimberlite Type Diamonds), Moscow: Nedra, 1994.