Original paper

Tomtor, the world's largest Sc-REE-Y-Nb-deposit

Kravchenko, S. M.

Global Tectonics and Metallogeny Volume 9 (2007), p. 31 - 37

26 references

published: Jan 1, 2007

BibTeX file

ArtNo. ESP136000900026, Price: 19.00 €

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The Tomtor Massif, which is exposed over an area of more than 250 km 2, belongs to the class of giant carbonatite-nepheline syenite massifs within the alkaline ultramafic association. The spatial restriction of the Tomtor Massif to a junction zone between mantle convective cells led us to suggest the existence of a giant longlived mantle plume. Such plume could bring mantle matter rich in different trace elements related to different metasomatic processes at different depths. The uniqueness of the Tomtor Sc-REE-Y-Nb deposit, which jointly contains both Nb and REE ore mineralisations, can be explained by the genetic relation of the complex to a K-Ca parent mantle magma.


tomtor massifcarbonatitenephelinealkalinemantle magma