Abstract
It has been shown that, in comparison with basalts, the products formed as a result of the processes of magma generation, earthquakes, volcanic activity, formation of lamproite and kimberlite tubes and others are enriched with light mantle elements.
This can be explained by the fact that the reason for the above processes is oxidation (combustion) of these elements because the macro quantities of some of mantle elements (Zi, Na, K, Rb, Cs, Mg, Ca, Sr, Ba, Al, and Si) are locally accumulated in the mantle and lithosphère. The elements with a high density, if separated from silicates, submerge mto the core. Some of them can enrich seismic activity products only under conditions permitting the arising of then volatile forms (sulphides, halogenides, and others).
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Chuburkov, Y.T. (2001). Chemical Nature of Seismic Phenomena. In: Frontasyeva, M.V., Perelygin, V.P., Vater, P. (eds) Radionuclides and Heavy Metals in Environment. NATO Science Series, vol 5. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-0993-5_37
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DOI: https://doi.org/10.1007/978-94-010-0993-5_37
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