Plume-related mantle source of super-large rare metal deposits from the Lovozero and Khibina massifs on the Kola Peninsula, Eastern part of Baltic Shield: Sr, Nd and Hf isotope systematics

Author:

Kogarko L. N.,Lahaye Y.,Brey G. P.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference50 articles.

1. Arndt NT, Christensen U (1992) The role of lithospheric mantle in continental flood volcanism: thermal and geochemical constraints. J Geophys Res 97:10967–10981

2. Arzamastsev AA, Arzamastseva LV, Glaznev VN, Raevskiy YA (1998) The deep structure and composition of the lower units of Khibiny and Lovozero complexes, Kola Peninsula, Russia: a petrological and geophysical model. Petrologiya 6:478–496

3. Bell K (2001) Carbonatites: relationship to mantle-plume activity. In: Ernst RE, Buchan KL (ed) Mantle plumes: the identification through time. Geological Society of America. Special Paper, 352:267–290

4. Bell K, Rukhlov AS (2004) Carbonatites from the Kola Alkaline Province: origin, evolution and source characteristics. In: Wall F, Zaitsev AN (eds) Phoscorites and carbonatites from mantle to mine. Mineral Soc Ser 10:433–468

5. Bizimis M, Salters V, Dawson JB (2003) The brevity of carbonatite sources in the mantle:evidence from Hf isotopes. Contrib Miner Petrol 145:281–300

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