Process mineralogy of rare earths from deeply weathered alkali-carbonatite deposits in Brazil

Brazil has the second largest rare earths mineral (REM) resource in the world, mainly associated with the weathered portion of carbonatite complexes. This paper reports process mineralogy studies performed for 10 samples collected from the deeply weathered portion of different relevant Brazilian dep...

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Main Authors: Juliana Lívi Antoniassi, Daniel Uliana, Renato Contessotto, Henrique Kahn, Carina Ulsen
Format: Article
Language:English
Published: Elsevier 2020-07-01
Series:Journal of Materials Research and Technology
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2238785420313983
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author Juliana Lívi Antoniassi
Daniel Uliana
Renato Contessotto
Henrique Kahn
Carina Ulsen
author_facet Juliana Lívi Antoniassi
Daniel Uliana
Renato Contessotto
Henrique Kahn
Carina Ulsen
author_sort Juliana Lívi Antoniassi
collection DOAJ
description Brazil has the second largest rare earths mineral (REM) resource in the world, mainly associated with the weathered portion of carbonatite complexes. This paper reports process mineralogy studies performed for 10 samples collected from the deeply weathered portion of different relevant Brazilian deposits, having a soil appearance and varied grain sizes with a significant content of natural fines (below 20 μm). The results indicate that REM are mainly composed of light rare earth elements and present a fine-grained nature and intricate associations with gangue minerals. Monazite is by far the most relevant REM; cerianite and bastnaesite are typical of only one of the studied deposits. The complexity of the occurrence of the rare earths challenges the development of mineral processing routes. A scandium phosphate mineral identified as a trace in one of the studied deposits has not yet been reported in the Brazilian alkaline complexes.
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spelling doaj.art-90d76a2edfe948bfa079bf2f0ad428b02022-12-21T23:16:34ZengElsevierJournal of Materials Research and Technology2238-78542020-07-019488428853Process mineralogy of rare earths from deeply weathered alkali-carbonatite deposits in BrazilJuliana Lívi Antoniassi0Daniel Uliana1Renato Contessotto2Henrique Kahn3Carina Ulsen4Corresponding author.; Universidade de São Paulo, Mining and Petroleum Engineering Department, Technological Characterization Laboratory (LCT-USP), Av. Prof. Mello Moraes, 2373, 05508-030 Sao Paulo, SP, BrazilUniversidade de São Paulo, Mining and Petroleum Engineering Department, Technological Characterization Laboratory (LCT-USP), Av. Prof. Mello Moraes, 2373, 05508-030 Sao Paulo, SP, BrazilUniversidade de São Paulo, Mining and Petroleum Engineering Department, Technological Characterization Laboratory (LCT-USP), Av. Prof. Mello Moraes, 2373, 05508-030 Sao Paulo, SP, BrazilUniversidade de São Paulo, Mining and Petroleum Engineering Department, Technological Characterization Laboratory (LCT-USP), Av. Prof. Mello Moraes, 2373, 05508-030 Sao Paulo, SP, BrazilUniversidade de São Paulo, Mining and Petroleum Engineering Department, Technological Characterization Laboratory (LCT-USP), Av. Prof. Mello Moraes, 2373, 05508-030 Sao Paulo, SP, BrazilBrazil has the second largest rare earths mineral (REM) resource in the world, mainly associated with the weathered portion of carbonatite complexes. This paper reports process mineralogy studies performed for 10 samples collected from the deeply weathered portion of different relevant Brazilian deposits, having a soil appearance and varied grain sizes with a significant content of natural fines (below 20 μm). The results indicate that REM are mainly composed of light rare earth elements and present a fine-grained nature and intricate associations with gangue minerals. Monazite is by far the most relevant REM; cerianite and bastnaesite are typical of only one of the studied deposits. The complexity of the occurrence of the rare earths challenges the development of mineral processing routes. A scandium phosphate mineral identified as a trace in one of the studied deposits has not yet been reported in the Brazilian alkaline complexes.http://www.sciencedirect.com/science/article/pii/S2238785420313983Rare earth elementsMonaziteBastnaesiteBrazilian depositsProcess mineralogy
spellingShingle Juliana Lívi Antoniassi
Daniel Uliana
Renato Contessotto
Henrique Kahn
Carina Ulsen
Process mineralogy of rare earths from deeply weathered alkali-carbonatite deposits in Brazil
Journal of Materials Research and Technology
Rare earth elements
Monazite
Bastnaesite
Brazilian deposits
Process mineralogy
title Process mineralogy of rare earths from deeply weathered alkali-carbonatite deposits in Brazil
title_full Process mineralogy of rare earths from deeply weathered alkali-carbonatite deposits in Brazil
title_fullStr Process mineralogy of rare earths from deeply weathered alkali-carbonatite deposits in Brazil
title_full_unstemmed Process mineralogy of rare earths from deeply weathered alkali-carbonatite deposits in Brazil
title_short Process mineralogy of rare earths from deeply weathered alkali-carbonatite deposits in Brazil
title_sort process mineralogy of rare earths from deeply weathered alkali carbonatite deposits in brazil
topic Rare earth elements
Monazite
Bastnaesite
Brazilian deposits
Process mineralogy
url http://www.sciencedirect.com/science/article/pii/S2238785420313983
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