ALTERATION OF SULFIDE ORES OF THE SAMOLAZOVSKOE DEPOSIT, ALDAN SHIELD, IN AN EXPERIMENTAL BIOLEACHING HEAP

The paper presents the results of a mineralogical study of sulfide ores of the Samolazovskoe deposit (Aldan Shield) and the products of their experimental bacterial oxidation in a heap. Pyrite and marcasite are the major minerals of primary ores. They form fine-grained crystalline and micrometer-gra...

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Main Authors: E.V. Belogub, K.A. Novoselov, I.B. Fadina, M.A. Rassomakhin
Format: Article
Language:English
Published: South Urals Federal Research Center of Mineralogy and Geoecology UB RAS 2023-03-01
Series:Минералогия
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Online Access:https://journal.mineralogy.ru/wp-content/uploads/2023/03/2023_9_1_3.pdf
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author E.V. Belogub
K.A. Novoselov
I.B. Fadina
M.A. Rassomakhin
author_facet E.V. Belogub
K.A. Novoselov
I.B. Fadina
M.A. Rassomakhin
author_sort E.V. Belogub
collection DOAJ
description The paper presents the results of a mineralogical study of sulfide ores of the Samolazovskoe deposit (Aldan Shield) and the products of their experimental bacterial oxidation in a heap. Pyrite and marcasite are the major minerals of primary ores. They form fine-grained crystalline and micrometer-grained to cryptocrystalline aggregates. Sphalerite, galena, chalcopyrite, pyrrhotite, fahlore, luzonite, bournonite and other Sb sulfosalts, stibnite and arsenopyrite are minor minerals. Tiemannite, coloradoite, calaverite, hessite, petzite and native gold are rare. The ores in the experimental biooxidation heap are mostly altered in its upper part. The secondary alteration products of ores include fine-grained Mg- and S-bearing calcite, smectites after feldspars, and films of Fe3+oxyhydroxides on the surface and in fractures of ore. In the lower part of the heap, technogenic processes are weak and are mainly related to the formation of gypsum. The sulfides are preserved throughout the heap vertical profile including very fine crystalline, colloform and botryoidal aggregates with a nonstoichiometric cation/anion ratio and the presence of As, Ni and Cu. The botryoidal aggregates of Fe disulfides contain galena, which forms a «microseptary» structure, which was not found in primary ores. The high-fineness native gold was found in assemblage with coloradoite and calaverite as inclusions in fine-grained aggregates of Fe disulfides. It is concluded on an insufficient impact of the bioleaching of refractory ores in an applied irrigation regime and the formation of secondary minerals that prevent the extraction of gold.
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institution Kabale University
issn 2313-545X
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language English
publishDate 2023-03-01
publisher South Urals Federal Research Center of Mineralogy and Geoecology UB RAS
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spelling doaj-art-ea8ff57ddbbb4153a0e33aa80f6715d32025-02-07T10:50:56ZengSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASМинералогия2313-545X2782-20442023-03-0191455910.35597/2313-545X-2023-9-1-3ALTERATION OF SULFIDE ORES OF THE SAMOLAZOVSKOE DEPOSIT, ALDAN SHIELD, IN AN EXPERIMENTAL BIOLEACHING HEAPE.V. Belogub0K.A. Novoselov1I.B. Fadina2M.A. Rassomakhin3South Urals Federal Research Center of Mineralogy and Geoecology UB RASSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASSeligdar CompanySouth Urals Federal Research Center of Mineralogy and Geoecology UB RASThe paper presents the results of a mineralogical study of sulfide ores of the Samolazovskoe deposit (Aldan Shield) and the products of their experimental bacterial oxidation in a heap. Pyrite and marcasite are the major minerals of primary ores. They form fine-grained crystalline and micrometer-grained to cryptocrystalline aggregates. Sphalerite, galena, chalcopyrite, pyrrhotite, fahlore, luzonite, bournonite and other Sb sulfosalts, stibnite and arsenopyrite are minor minerals. Tiemannite, coloradoite, calaverite, hessite, petzite and native gold are rare. The ores in the experimental biooxidation heap are mostly altered in its upper part. The secondary alteration products of ores include fine-grained Mg- and S-bearing calcite, smectites after feldspars, and films of Fe3+oxyhydroxides on the surface and in fractures of ore. In the lower part of the heap, technogenic processes are weak and are mainly related to the formation of gypsum. The sulfides are preserved throughout the heap vertical profile including very fine crystalline, colloform and botryoidal aggregates with a nonstoichiometric cation/anion ratio and the presence of As, Ni and Cu. The botryoidal aggregates of Fe disulfides contain galena, which forms a «microseptary» structure, which was not found in primary ores. The high-fineness native gold was found in assemblage with coloradoite and calaverite as inclusions in fine-grained aggregates of Fe disulfides. It is concluded on an insufficient impact of the bioleaching of refractory ores in an applied irrigation regime and the formation of secondary minerals that prevent the extraction of gold.https://journal.mineralogy.ru/wp-content/uploads/2023/03/2023_9_1_3.pdf: samolazovskoe depositaldan shieldcoloradoitecalaveritenative goldrefractory oresbiooxidation
spellingShingle E.V. Belogub
K.A. Novoselov
I.B. Fadina
M.A. Rassomakhin
ALTERATION OF SULFIDE ORES OF THE SAMOLAZOVSKOE DEPOSIT, ALDAN SHIELD, IN AN EXPERIMENTAL BIOLEACHING HEAP
Минералогия
: samolazovskoe deposit
aldan shield
coloradoite
calaverite
native gold
refractory ores
biooxidation
title ALTERATION OF SULFIDE ORES OF THE SAMOLAZOVSKOE DEPOSIT, ALDAN SHIELD, IN AN EXPERIMENTAL BIOLEACHING HEAP
title_full ALTERATION OF SULFIDE ORES OF THE SAMOLAZOVSKOE DEPOSIT, ALDAN SHIELD, IN AN EXPERIMENTAL BIOLEACHING HEAP
title_fullStr ALTERATION OF SULFIDE ORES OF THE SAMOLAZOVSKOE DEPOSIT, ALDAN SHIELD, IN AN EXPERIMENTAL BIOLEACHING HEAP
title_full_unstemmed ALTERATION OF SULFIDE ORES OF THE SAMOLAZOVSKOE DEPOSIT, ALDAN SHIELD, IN AN EXPERIMENTAL BIOLEACHING HEAP
title_short ALTERATION OF SULFIDE ORES OF THE SAMOLAZOVSKOE DEPOSIT, ALDAN SHIELD, IN AN EXPERIMENTAL BIOLEACHING HEAP
title_sort alteration of sulfide ores of the samolazovskoe deposit aldan shield in an experimental bioleaching heap
topic : samolazovskoe deposit
aldan shield
coloradoite
calaverite
native gold
refractory ores
biooxidation
url https://journal.mineralogy.ru/wp-content/uploads/2023/03/2023_9_1_3.pdf
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AT kanovoselov alterationofsulfideoresofthesamolazovskoedepositaldanshieldinanexperimentalbioleachingheap
AT ibfadina alterationofsulfideoresofthesamolazovskoedepositaldanshieldinanexperimentalbioleachingheap
AT marassomakhin alterationofsulfideoresofthesamolazovskoedepositaldanshieldinanexperimentalbioleachingheap