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Global tectonic settings and deep mantle control on Hg and Au-Hg deposits

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Mineral Deposit Research: Meeting the Global Challenge

Abstract

Three main geodynamic environments are favorable for the development of ore-forming systems of Hg and Au-Hg deposits: Intracontinental rifts and aulacogens at the ancient cratons, intraplate rifting in the orogenic belts of different ages, and active continental margins of the continents. The isotope-geochemical characteristics of ore-forming systems of Hg and Au-Hg deposits, changes in 3He/4Hg ratio, and paragenetic relationship between subcrustal basite and alkaline basite magmatism suggest that mantle plumes played a significant role in their formation.

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© 2005 Springer-Verlag Berlin Heidelberg

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Borisenko, A.S., Obolenskiy, A.A., Naumov, E.A. (2005). Global tectonic settings and deep mantle control on Hg and Au-Hg deposits. In: Mao, J., Bierlein, F.P. (eds) Mineral Deposit Research: Meeting the Global Challenge. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-27946-6_1

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