Author:
Prokofiev V. Yu.,Banks D. A.,Lobanov K. V.,Selektor S. L.,Milichko V. A.,Akinfiev N. N.,Borovikov A. A.,Lüders V.,Chicherov M. V.
Abstract
AbstractIn the drill core of the Kola super-deep borehole (SG-3, 12,262 m depth) gold-bearing rocks of Archaean age have been located at depths of 9,500 to 11,000 m. In veins, between 9,052 and 10,744 m, within this gold zone, quartz contains fluid inclusions with gold nanoparticles. There are 4 types of fluid inclusions (1) gas inclusions of dense CO2, (2) liquid-vapor two-phase aqueous inclusions, (3) three-phase inclusions with NaCl daughter crystals, and (4) CO2-aqueous inclusions. In all inclusion types, there are extremely high concentrations of gold. The highest gold concentrations were found in the type 3 and 4 fluid inclusions with an average concentration of c. 750 ppm and may be as high as 6,000 ppm. The presence of gold as nanoparticles in the solutions of these fluid inclusions was determined by optical and spectroscopic methods. We suggest that these fluids could be a precursor of “orogenic gold fluids” which, at the gold concentrations determined, would reduce the requirements for large volumes of metamorphic fluids to form orogenic ore deposits. Further, as nanoparticles, gold could be transported in larger amounts than in true solution.
Publisher
Springer Science and Business Media LLC
Reference66 articles.
1. Groves, D. I. et al. Orogenic gold deposits: A proposed classification in the context of their crustal distribution and relationship to other gold deposit types. Ore Geology Rev. 13, 7–27 (1998).
2. Goldfarb, R. J. et al. Distribution, character, and genesis of gold deposits in metamorphic terranes. Economic Geology 100th Anniversary Volume. 407–450 (2005).
3. Goldfarb, R. J. & Groves, D. I. Orogenic gold: Common or evolving fluid and metal sources through time. Lithos. 233, 2–26 (2015).
4. Pitcairn, I. K., Craw, D. & Teagle, D. A. H. The gold conveyer belt: Large scale gold mobility in an active orogen. Ore Geology Reviews. 62, 129–142 (2014).
5. Ward, J., Mavrogenes, J., Murray, A. & Holden, P. Trace element and sulfur isotopic evidence for redox changes during formation of the Wallaby Gold Deposit, Western Australia. Ore Geology Reviews. 82, 31–48 (2017).
Cited by
19 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献