Kimberlite occurrences within an 85 x 60 km physical and geological inhomogeneity at the eastern margin of the East European Platform. This inhomogeneity is interpreted as a near-vertical domain of mantle and crustal material transformed by the development of a kimberlite system. In addition to tens of kimberlite pipes, olivine melilitites and basalts occur in this area.
References
- Kononova, V.A., Golubeva, Y.Y., Bogatikov, O.A., and Kargin, A.V. (2007): Diamond Resource Potential of Kimberlites from the Zimny Bereg Field, Arkhangel’sk Oblast. Geology of Ore Deposits 49(6), 421-441.
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