Petrographic characteristic of bauxites of the Koulore ore field

As a result of studying geological structure of deposits located in the Koulore ore field, basic cross-section layers have been established: bedrock, transitional horizon and laterite cover. The laterite cover consists of the lower part presented by polymineral and kaolin clays and the top - the bau...

Full description

Bibliographic Details
Main Authors: Lucien Toure, Alexey A Chausov, Alexander E Kotelnikov
Format: Article
Language:English
Published: Peoples’ Friendship University of Russia (RUDN University) 2018-12-01
Series:RUDN Journal of Engineering Research
Subjects:
Online Access:http://journals.rudn.ru/engineering-researches/article/viewFile/19254/16105
_version_ 1797936851522158592
author Lucien Toure
Alexey A Chausov
Alexander E Kotelnikov
author_facet Lucien Toure
Alexey A Chausov
Alexander E Kotelnikov
author_sort Lucien Toure
collection DOAJ
description As a result of studying geological structure of deposits located in the Koulore ore field, basic cross-section layers have been established: bedrock, transitional horizon and laterite cover. The laterite cover consists of the lower part presented by polymineral and kaolin clays and the top - the bauxite horizon - laterite cover itself, which generally contains hydroxides and oxides of iron and aluminum. The bauxite horizon has a zone structure: in the lower part of the bauxite horizon - zone of light bauxites, and in the top part of the bauxite horizon - zone of the red bauxites. As a result of microscopic study of various samples of residuum, several kinds of rocks which are characterized by similar structural and textural parameters have been identified. The rocks have been grouped by classes: gelified patterned bauxites on silt-rich mudstone, gelified bauxites on dolerites, gel-morphous bauxites with crystalloids on silt-rich mudstone, laterite bauxites (low-quality bauxites) on silt-rich mudstone, laterite bauxites (low-quality bauxites) on dolerites, ferruginous laterites - cuirass on silt-rich mudstone, ferruginous laterites of the top part of the transitional horizon on silt-rich mudstone. Lithological and genetic types of bauxites control the type and composition of aluminiferous minerals. Mineral composition of classical lateritic bauxites mainly contains gibbsite, goethite-alumogoethite, and hematite with less 1% of boehmite. Gel-morphous and gelified bauxites consist of gibbsite, boehmite, goethite-alumogoethite, hematite. Content of boehmite reaches 3% that is more than in classic lateritic bauxites. The composition of the alumogoethite depends not only on lithology of bauxites, but also on position in the residuum section.
first_indexed 2024-04-10T18:36:41Z
format Article
id doaj.art-c0094e926db54b55b043fce9f7891f64
institution Directory Open Access Journal
issn 2312-8143
2312-8151
language English
last_indexed 2024-04-10T18:36:41Z
publishDate 2018-12-01
publisher Peoples’ Friendship University of Russia (RUDN University)
record_format Article
series RUDN Journal of Engineering Research
spelling doaj.art-c0094e926db54b55b043fce9f7891f642023-02-02T01:15:13ZengPeoples’ Friendship University of Russia (RUDN University)RUDN Journal of Engineering Research2312-81432312-81512018-12-0119332534210.22363/2312-8143-2018-19-3-325-34216770Petrographic characteristic of bauxites of the Koulore ore fieldLucien Toure0Alexey A Chausov1Alexander E Kotelnikov2Peoples’ Friendship University of Russia (RUDN University)Geoprospects LTDPeoples’ Friendship University of Russia (RUDN University)As a result of studying geological structure of deposits located in the Koulore ore field, basic cross-section layers have been established: bedrock, transitional horizon and laterite cover. The laterite cover consists of the lower part presented by polymineral and kaolin clays and the top - the bauxite horizon - laterite cover itself, which generally contains hydroxides and oxides of iron and aluminum. The bauxite horizon has a zone structure: in the lower part of the bauxite horizon - zone of light bauxites, and in the top part of the bauxite horizon - zone of the red bauxites. As a result of microscopic study of various samples of residuum, several kinds of rocks which are characterized by similar structural and textural parameters have been identified. The rocks have been grouped by classes: gelified patterned bauxites on silt-rich mudstone, gelified bauxites on dolerites, gel-morphous bauxites with crystalloids on silt-rich mudstone, laterite bauxites (low-quality bauxites) on silt-rich mudstone, laterite bauxites (low-quality bauxites) on dolerites, ferruginous laterites - cuirass on silt-rich mudstone, ferruginous laterites of the top part of the transitional horizon on silt-rich mudstone. Lithological and genetic types of bauxites control the type and composition of aluminiferous minerals. Mineral composition of classical lateritic bauxites mainly contains gibbsite, goethite-alumogoethite, and hematite with less 1% of boehmite. Gel-morphous and gelified bauxites consist of gibbsite, boehmite, goethite-alumogoethite, hematite. Content of boehmite reaches 3% that is more than in classic lateritic bauxites. The composition of the alumogoethite depends not only on lithology of bauxites, but also on position in the residuum section.http://journals.rudn.ru/engineering-researches/article/viewFile/19254/16105residuum sectionbauxitelateritepetrography
spellingShingle Lucien Toure
Alexey A Chausov
Alexander E Kotelnikov
Petrographic characteristic of bauxites of the Koulore ore field
RUDN Journal of Engineering Research
residuum section
bauxite
laterite
petrography
title Petrographic characteristic of bauxites of the Koulore ore field
title_full Petrographic characteristic of bauxites of the Koulore ore field
title_fullStr Petrographic characteristic of bauxites of the Koulore ore field
title_full_unstemmed Petrographic characteristic of bauxites of the Koulore ore field
title_short Petrographic characteristic of bauxites of the Koulore ore field
title_sort petrographic characteristic of bauxites of the koulore ore field
topic residuum section
bauxite
laterite
petrography
url http://journals.rudn.ru/engineering-researches/article/viewFile/19254/16105
work_keys_str_mv AT lucientoure petrographiccharacteristicofbauxitesofthekouloreorefield
AT alexeyachausov petrographiccharacteristicofbauxitesofthekouloreorefield
AT alexanderekotelnikov petrographiccharacteristicofbauxitesofthekouloreorefield