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Mantle magma-thermofluidodynamic and intracrustal granitoid-hydrothermal-metasomatic auriferous systems

Authors: Korobeynikov, A. F.;

Mantle magma-thermofluidodynamic and intracrustal granitoid-hydrothermal-metasomatic auriferous systems

Abstract

Contents of typical models of formation of abyssal and intra-core ore-forming systems are discussed. As it has been already marked, the interaction between core and mantle ore-forming systems occurred at formation of large and unique golden-ore deposits. The interaction of the abyssal mantle substance with formations of the Earth's crust has been carried out by penetration of high-temperature gas-fluids, magmatic melts and solid bodies, forming diapiric magma-thermofluidodynamic systems on borders of the inner core with the bottom mantle and within the limits of the upper mantle - the Earth's crust

Country
Russian Federation
Related Organizations
Keywords

auriferous systems, ore-forming systems, magmatic melts, golden-ore deposits, solid bodies, gas-fluids, granitoid-hydrothermal-metasomatic auriferous systems, Earth's crust, mantle, mantle magma-thermofluidodynamic auriferous systems

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citations
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Citations provided by BIP!
popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
0
Average
Average
Average
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