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.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
