Lead isotopic evidence for interaction between plume and lower crust during emplacement of peralkaline Lovozero rocks and related rare-metal deposits, East Fennoscandia, Kola Peninsula, Russia

Author:

Zartman R. E.,Kogarko L. N.

Funder

Russian Science Foundation

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference61 articles.

1. Amelin YV, Neymark LA (1998) Lead isotope geochemistry of Paleoproterozoic layered intrusions in the eastern Baltic Shield: Inferences about magma sources and U-Th-Pb fractionation in the crust-mantle system. Geochim Cosmochim Acta 62:493–505

2. Arzamastsev AA, Bea F, Glaznev VN, Arzamastseva LV, Montero P (2001) Kola alkaline province in the Paleozoic: evaluation of primary mantle magma composition and magma generation conditions. Russ J Earth Sci 3:3–24

3. Arzamastsev AA, Arzamastseva LV, Glaznev VN, Raevskiy YuA (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

4. Bayanova T, Ludden J, Mitrofanov F (2009) Timing and duration of Palaeoproterozoic events producing ore-bearing layered intrusions of the Baltic Shield: metallogenic, petrological and geodynamic implications. Geol Soc Lond 323:165–198

5. 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, 10. Mineralogical Society, Washington, DC, pp 433–468

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