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A. S. Vakh
Russian Academy of Sciences
GeomorphologyGeologyGeochemistryEarth (classical element)Mineralization (biology)
14Publications
2H-index
10Citations
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Publications 17
Newest
#1V. I. GvozdevH-Index: 3
Last. D. G. FedoseevH-Index: 2
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#1A. S. VakhH-Index: 2
#2V. I. GvozdevH-Index: 3
Last. E. A. VakhH-Index: 1
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#1A. S. Vakh (RAS: Russian Academy of Sciences)H-Index: 2
#2O. V. Avchenko (RAS: Russian Academy of Sciences)H-Index: 4
Last. E. A. VakhH-Index: 1
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The composition and genesis of Pb–As–Sb sulfosalts from ores of the Berezitovoe gold deposit, Upper Amur Region, located in the eastern part of the Mongolia-Okhotsk orogenic belt are reported. Lead (Pb–Cu) sulfosalts are tsugaruite, dufrenoysite, boulangerite, menegenite, Bi-rich menegenite (Bi up to 11.5 wt %), and minerals of the jordanite-geocronite and bournonite-seligmannite solid solution series. Basic features of the relationship between Pb sulfosalts and ore and silicate minerals in vari...
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#1E. A. Vakh (RAS: Russian Academy of Sciences)H-Index: 1
#2A. S. Vakh (RAS: Russian Academy of Sciences)H-Index: 2
Last. N. N. Barinov (RAS: Russian Academy of Sciences)H-Index: 3
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The REE composition of modern mineral–organic associations in the sulfide ore hypergenesis zone of the Berezitovoe deposit in the Russian Far East was studied for the first time. It is shown that the mineral–organic associations widely abundant in the valley of Konstantinovskii Creek and represented by bright brown crusts on the surface of deluvial deposits were formed at the expense of the influence of acid highly mineralized mine waters from the Berezitovoe deposit. The mineral–organic associa...
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#1A. S. VakhH-Index: 2
#3V. I. GvozdevH-Index: 3
Last. E. A. VakhH-Index: 1
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#1E. A. VakhH-Index: 1
#2V. I. PetukhovH-Index: 1
Last. A. S. ZubtsovaH-Index: 1
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#1A. S. Vakh (RAS: Russian Academy of Sciences)H-Index: 2
#2O. V. Avchenko (RAS: Russian Academy of Sciences)H-Index: 4
Last. E. A. VakhH-Index: 1
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New data are presented on segregations and compositions of bournonite-seligmannite series of minerals in gold-bearing veinlets of the Beresitovoe deposit located in the eastern part of the Mongolia–Okhotsk Orogenic Belt. It was established that these minerals represent a discrete series of stoichiometric solid compounds with As formula coefficients varying from 0.2 to 1.2. It is shown that minerals of this series are characteristic of ore deposits that undergo high-grade metamorphism, the P–T co...
1 CitationsSource
#1Guobin Zhang (Liaoning Technical University)H-Index: 1
#2Yanchen Yang (JLU: Jilin University)H-Index: 2
Last. Shijiong Han (JLU: Jilin University)H-Index: 1
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#1E. A. VakhH-Index: 1
#2A. S. VakhH-Index: 2
Last. A. S. ZubtsovaH-Index: 1
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1 CitationsSource
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