NEW RESULTS ON THE GEOLOGY OF THE LOVOZERO MASSIF

Abstract
New data collected since 1955 on the geology of the Lovozero massif, considerably detailing and supplementing existing ideas as to its structure and geochemistry, are presented. As a result of these investigations the thickness of the ore-bearing stratified rock complex has been traced to a depth of 1700 m. Laws governing the vertical alteration of rock composition of individual series have been established as well as the fact that the amount of titanium-bearing minerals increases with depth.—Auth. English summ.

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