The geochemical features of ores and technosoils of tailing gold-molybdenum mine Davenda in East Transbaikalia
New data on the mineral and chemical composition of the ore, host rocks and technosoils of tailings gold-molybdenum deposit Davenda are outlined. The mineral composition of the ore (%): quartz (96), molybdenite (1, but on average 0.26), pyrite (7), chalcopyrite (2), sphalerite (0.07), galena (to.1),...
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A.N. Zavaritsky Institute of Geology and Geochemistry
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doaj-58eb2b816a1f404181e13c97f263e8282020-11-25T03:52:18ZengA.N. Zavaritsky Institute of Geology and GeochemistryЛитосфера1681-90042500-302X2016-04-01029110618The geochemical features of ores and technosoils of tailing gold-molybdenum mine Davenda in East TransbaikaliaG. A. Yurgenson0O. K. Smirnova1M. A. Solodukhina2R. A. Filenko3The Institute of Natural Resources, Ecology, and Cryology, Siberian Branch of RASGeological institute of the Siberian Branch of RASThe Institute of Natural Resources, Ecology, and Cryology, Siberian Branch of RASThe Institute of Natural Resources, Ecology, and Cryology, Siberian Branch of RASNew data on the mineral and chemical composition of the ore, host rocks and technosoils of tailings gold-molybdenum deposit Davenda are outlined. The mineral composition of the ore (%): quartz (96), molybdenite (1, but on average 0.26), pyrite (7), chalcopyrite (2), sphalerite (0.07), galena (to.1), sulphosalts (0.02), bismuthinite (0.2), scheelite (up to 0.02), tungsten (up to 0.01), bornite (0.03), tetradymite (to 0.001) emplektite (rare occurrences) and gold (up to1817g/t). In the oxidation zone developed various sulfates, including large (up to10 cm) gypsum crystals, chalkanthite, malachite, azurite, brochantite, molybdenite, ferrimolybdite. The contents of the main chemical elements, which compose technosoils of tailing, exeed their clarks. Exceptions are zinc, tin, and yttrium. Especially high concentration factors for arsenic, bismuth and molybdenum, which indicates the imperfection of applied technologies of the ores enrichment. The distribution of chemical elements in the geotechnogenic system: productive mineral complex (ore + host rock)→soil→technosoils →plants. Revealed the share of Mo, Zn, Cu, Pb mobile form, in technosoils. Identified acid-base characteristics of technosoils. It was found that the most important of the mobile forms is a water-acid-ion exchange, to a much lesser extent - organic elements.https://www.lithosphere.ru/jour/article/view/18золото-молибденовая рудатехноземхвостохранилищехимический элементподвижная формакоэффициент биологического поглощениядавендинское месторождениевосточное забайкальеgold-molybdenum oretechnosoiltailinga chemical elementthe mobile formfactor of biological absorptiondeposit davendaeastern transbaikalia |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
G. A. Yurgenson O. K. Smirnova M. A. Solodukhina R. A. Filenko |
spellingShingle |
G. A. Yurgenson O. K. Smirnova M. A. Solodukhina R. A. Filenko The geochemical features of ores and technosoils of tailing gold-molybdenum mine Davenda in East Transbaikalia Литосфера золото-молибденовая руда технозем хвостохранилище химический элемент подвижная форма коэффициент биологического поглощения давендинское месторождение восточное забайкалье gold-molybdenum ore technosoil tailing a chemical element the mobile form factor of biological absorption deposit davenda eastern transbaikalia |
author_facet |
G. A. Yurgenson O. K. Smirnova M. A. Solodukhina R. A. Filenko |
author_sort |
G. A. Yurgenson |
title |
The geochemical features of ores and technosoils of tailing gold-molybdenum mine Davenda in East Transbaikalia |
title_short |
The geochemical features of ores and technosoils of tailing gold-molybdenum mine Davenda in East Transbaikalia |
title_full |
The geochemical features of ores and technosoils of tailing gold-molybdenum mine Davenda in East Transbaikalia |
title_fullStr |
The geochemical features of ores and technosoils of tailing gold-molybdenum mine Davenda in East Transbaikalia |
title_full_unstemmed |
The geochemical features of ores and technosoils of tailing gold-molybdenum mine Davenda in East Transbaikalia |
title_sort |
geochemical features of ores and technosoils of tailing gold-molybdenum mine davenda in east transbaikalia |
publisher |
A.N. Zavaritsky Institute of Geology and Geochemistry |
series |
Литосфера |
issn |
1681-9004 2500-302X |
publishDate |
2016-04-01 |
description |
New data on the mineral and chemical composition of the ore, host rocks and technosoils of tailings gold-molybdenum deposit Davenda are outlined. The mineral composition of the ore (%): quartz (96), molybdenite (1, but on average 0.26), pyrite (7), chalcopyrite (2), sphalerite (0.07), galena (to.1), sulphosalts (0.02), bismuthinite (0.2), scheelite (up to 0.02), tungsten (up to 0.01), bornite (0.03), tetradymite (to 0.001) emplektite (rare occurrences) and gold (up to1817g/t). In the oxidation zone developed various sulfates, including large (up to10 cm) gypsum crystals, chalkanthite, malachite, azurite, brochantite, molybdenite, ferrimolybdite. The contents of the main chemical elements, which compose technosoils of tailing, exeed their clarks. Exceptions are zinc, tin, and yttrium. Especially high concentration factors for arsenic, bismuth and molybdenum, which indicates the imperfection of applied technologies of the ores enrichment. The distribution of chemical elements in the geotechnogenic system: productive mineral complex (ore + host rock)→soil→technosoils →plants. Revealed the share of Mo, Zn, Cu, Pb mobile form, in technosoils. Identified acid-base characteristics of technosoils. It was found that the most important of the mobile forms is a water-acid-ion exchange, to a much lesser extent - organic elements. |
topic |
золото-молибденовая руда технозем хвостохранилище химический элемент подвижная форма коэффициент биологического поглощения давендинское месторождение восточное забайкалье gold-molybdenum ore technosoil tailing a chemical element the mobile form factor of biological absorption deposit davenda eastern transbaikalia |
url |
https://www.lithosphere.ru/jour/article/view/18 |
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