Zobrazeno 1 - 6
of 6
pro vyhledávání: '"classic lateritic bauxites"'
Autor:
Mamedov, Vladimir1 (AUTHOR) frolikovam@gmail.com, Boeva, Natalia1 (AUTHOR) boeva@igem.ru, Makarova, Marina1 (AUTHOR) filimon.mel@bk.ru, Shipilova, Elena1 (AUTHOR), Melnikov, Philimon1,2 (AUTHOR)
Publikováno v:
Minerals (2075-163X). Mar2022, Vol. 12 Issue 3, p389. 18p.
В статье рассмотрены условия и особенности формирования и распространения разнообразных по составу, строению и генезису бокситоносных
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::17b0834e830c52c179bff853ba5aa7d6
Publikováno v:
RUDN Journal of Engineering Research, Vol 19, Iss 3, Pp 325-342 (2018)
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
Externí odkaz:
https://doaj.org/article/c0094e926db54b55b043fce9f7891f64
Publikováno v:
Minerals; Volume 12; Issue 3; Pages: 389
The study of a large amount of factual material about the formation conditions of gibbsite or boehmite and their mutual transformations in lateritic bauxites allowed us to solve the problem of boehmite formation and its spatial and genetic relationsh
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4301b54a080fe23db2990a0cef22699c
Publikováno v:
Geology of Ore Deposits; Jun2011, Vol. 53 Issue 3, p177-201, 25p
Publikováno v:
RUDN Journal of Engineering Researches, Vol 19, Iss 3, Pp 325-342 (2018)
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::93ee79bfbcab555b6b078efde818f7e3
https://doi.org/10.22363/2312-8143-2018-19-3-325-342
https://doi.org/10.22363/2312-8143-2018-19-3-325-342