Abstract

The obtained evidence of hot heterogeneous accretion of the Earth leads to a fundamentally new solution to genetic problems. According to these data, the kimberlites were formed as a result of the rise of the last residual melts of the bottom peridotite layer of the magmatic ocean, which arose as a result of impact heat release during accretion. The diamond crystallized due to the accumulation of carbon in the residual melts during fractionation. The absence of kimberlites in oceanic and collision regions is due to the expansion of the fractionation products of the magmatic ocean by surfaced mantle plumes during the formation of these regions. The all-earth distribution of the magmatic ocean explains the presence of kimberlites on all the studied ancient platforms. A very high degree of crystallization of the peridotite layer is the reason for the small volume of kimberlite residual melts and the bodies formed by them. The low temperature of kimberlite magmas caused their decompression solidification after boiling at the shallow stage of ascent and explosion under the influence of the high pressure of the fluid phase preserved by solidification. This is the reason for the formation of kimberlite pipes and the absence of kimberlite lavas.

Highlights

  • Vladimir ShkodzinskyDiamond and Precious Metals Geology Institute of Siberian Branch of the Russian Academy of Sciences (IGABM SB RAS), Yakutsk, Russia

  • Finding out the patterns of kimberlite placement and their nature is of fundamental importance for the successful prediction and search for diamond deposits

  • This origin of diamonds is confirmed by the evolution of the composition of mineral inclusions in them from peridotite paragenesis to eclogite, pyroxenite and to kimberlite [3] and an increase in the content of impurities accumulated in the residual melts of chemical components, including nitrogen and a light carbon isotope, by thousands of times from early diamonds to late ones

Read more

Summary

Vladimir Shkodzinsky

Diamond and Precious Metals Geology Institute of Siberian Branch of the Russian Academy of Sciences (IGABM SB RAS), Yakutsk, Russia. Email address: To cite this article: Vladimir Shkodzinsky. Nature of the Features of Kimberlite Placement.

Introduction
Findings
Conclusion
Full Text
Published version (Free)

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 call