The Geology, Geochemistry, and Mineralogy of the Moa Bay Ni Laterite Mining District, Cuba
The Moa Bay lateritic Ni-Co mining district (eastern Cuba) has total mineral resources of 198.54 million metric tonnes (Mt) at 1.07% Ni and 0.12% Co. Laterite profiles from this district are characterized by their oxide-dominated ore zones. Laterite profiles from the Yagrumaje Norte, Punta Gorda, an...
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| Tipo de recurso: | artículo |
| Estado: | Versión aceptada para publicación |
| Fecha de publicación: | 2024 |
| País: | España |
| Institución: | Universidad de Barcelona |
| Repositorio: | Dipòsit Digital de la UB |
| OAI Identifier: | oai:diposit.ub.edu:2445/227510 |
| Acceso en línea: | https://hdl.handle.net/2445/227510 |
| Access Level: | acceso abierto |
| Palabra clave: | Geoquímica Mineralogia Níquel Cobalt Cuba Geochemistry Mineralogy Nickel |
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The Geology, Geochemistry, and Mineralogy of the Moa Bay Ni Laterite Mining District, CubaDomínguez-Carretero, DiegoProenza Fernández, Joaquín AntonioVillanova de Benavent, CristinaAiglsperger, Thomas HansTauler i Ferré, EsperançaRojas-Purón, ArturoDuque-Garcés, NathaliaGonzález Jiménez, José MaríaGarcia-Casco, AntonioGalí Medina, Salvador, 1949-GeoquímicaMineralogiaNíquelCobaltCubaGeochemistryMineralogyNickelCobaltCubaThe Moa Bay lateritic Ni-Co mining district (eastern Cuba) has total mineral resources of 198.54 million metric tonnes (Mt) at 1.07% Ni and 0.12% Co. Laterite profiles from this district are characterized by their oxide-dominated ore zones. Laterite profiles from the Yagrumaje Norte, Punta Gorda, and Yamanigüey deposits contain average Ni and Co concentrations in the oxide zone of 0.88 and 0.12%. Goethite is the most abundant mineral in the oxide zone and the most important Ni-Co-Sc–bearing mineral, with median NiO, CoO, and Sc contents of 0.78 wt %, 0.07 wt %, and 58 ppm, respectively, and up to 2.77 wt %, 0.26 wt %, and 117 ppm. Maghemite is also widely present (avg of 5% and up to 19% modal proportion) and represents an important but largely ignored Ni- and Co-bearing ore phase, with median NiO and CoO concentrations of 2.11 and 0.25 wt %, respectively, and maximum values of 13.9 and 1.84 wt % each. Nickel and Co substitute for ferric iron in the structure of maghemite. Manganese oxyhydroxides (lithiophorite and lithiophorite-asbolane intermediate), which are also significant Ni-Co–bearing phases, have median NiO and CoO contents of 10.6 and 6.41 wt %, respectively. Some Mn oxyhydroxides, which formed after replacing goethite, also contain significant amounts of Sc (up to 94 ppm). Although most deposits in the Moa Bay lateritic district are classified as oxide type, Yamanigüey (avg Ni grade of 1.98%) is characterized by well-developed saprolite horizons, with secondary serpentine (serpentine II) and garnierite being the main Ni-bearing phases.Society of Economic Geologists2024info:eu-repo/semantics/articleinfo:eu-repo/semantics/acceptedVersionapplication/pdfhttps://hdl.handle.net/2445/227510Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)reponame:Dipòsit Digital de la UBinstname:Universidad de BarcelonaInglésVersió postprint del document publicat a: https://doi.org/10.5382/econgeo.5101Economic Geology, 2024, vol. 119, num.7, p. 1685-1706https://doi.org/10.5382/econgeo.5101(c) Society of Economic Geologists, 2024info:eu-repo/semantics/openAccessoai:diposit.ub.edu:2445/2275102026-05-27T06:46:51Z |
| dc.title.none.fl_str_mv |
The Geology, Geochemistry, and Mineralogy of the Moa Bay Ni Laterite Mining District, Cuba |
| title |
The Geology, Geochemistry, and Mineralogy of the Moa Bay Ni Laterite Mining District, Cuba |
| spellingShingle |
The Geology, Geochemistry, and Mineralogy of the Moa Bay Ni Laterite Mining District, Cuba Domínguez-Carretero, Diego Geoquímica Mineralogia Níquel Cobalt Cuba Geochemistry Mineralogy Nickel Cobalt Cuba |
| title_short |
The Geology, Geochemistry, and Mineralogy of the Moa Bay Ni Laterite Mining District, Cuba |
| title_full |
The Geology, Geochemistry, and Mineralogy of the Moa Bay Ni Laterite Mining District, Cuba |
| title_fullStr |
The Geology, Geochemistry, and Mineralogy of the Moa Bay Ni Laterite Mining District, Cuba |
| title_full_unstemmed |
The Geology, Geochemistry, and Mineralogy of the Moa Bay Ni Laterite Mining District, Cuba |
| title_sort |
The Geology, Geochemistry, and Mineralogy of the Moa Bay Ni Laterite Mining District, Cuba |
| dc.creator.none.fl_str_mv |
Domínguez-Carretero, Diego Proenza Fernández, Joaquín Antonio Villanova de Benavent, Cristina Aiglsperger, Thomas Hans Tauler i Ferré, Esperança Rojas-Purón, Arturo Duque-Garcés, Nathalia González Jiménez, José María Garcia-Casco, Antonio Galí Medina, Salvador, 1949- |
| author |
Domínguez-Carretero, Diego |
| author_facet |
Domínguez-Carretero, Diego Proenza Fernández, Joaquín Antonio Villanova de Benavent, Cristina Aiglsperger, Thomas Hans Tauler i Ferré, Esperança Rojas-Purón, Arturo Duque-Garcés, Nathalia González Jiménez, José María Garcia-Casco, Antonio Galí Medina, Salvador, 1949- |
| author_role |
author |
| author2 |
Proenza Fernández, Joaquín Antonio Villanova de Benavent, Cristina Aiglsperger, Thomas Hans Tauler i Ferré, Esperança Rojas-Purón, Arturo Duque-Garcés, Nathalia González Jiménez, José María Garcia-Casco, Antonio Galí Medina, Salvador, 1949- |
| author2_role |
author author author author author author author author author |
| dc.subject.none.fl_str_mv |
Geoquímica Mineralogia Níquel Cobalt Cuba Geochemistry Mineralogy Nickel Cobalt Cuba |
| topic |
Geoquímica Mineralogia Níquel Cobalt Cuba Geochemistry Mineralogy Nickel Cobalt Cuba |
| description |
The Moa Bay lateritic Ni-Co mining district (eastern Cuba) has total mineral resources of 198.54 million metric tonnes (Mt) at 1.07% Ni and 0.12% Co. Laterite profiles from this district are characterized by their oxide-dominated ore zones. Laterite profiles from the Yagrumaje Norte, Punta Gorda, and Yamanigüey deposits contain average Ni and Co concentrations in the oxide zone of 0.88 and 0.12%. Goethite is the most abundant mineral in the oxide zone and the most important Ni-Co-Sc–bearing mineral, with median NiO, CoO, and Sc contents of 0.78 wt %, 0.07 wt %, and 58 ppm, respectively, and up to 2.77 wt %, 0.26 wt %, and 117 ppm. Maghemite is also widely present (avg of 5% and up to 19% modal proportion) and represents an important but largely ignored Ni- and Co-bearing ore phase, with median NiO and CoO concentrations of 2.11 and 0.25 wt %, respectively, and maximum values of 13.9 and 1.84 wt % each. Nickel and Co substitute for ferric iron in the structure of maghemite. Manganese oxyhydroxides (lithiophorite and lithiophorite-asbolane intermediate), which are also significant Ni-Co–bearing phases, have median NiO and CoO contents of 10.6 and 6.41 wt %, respectively. Some Mn oxyhydroxides, which formed after replacing goethite, also contain significant amounts of Sc (up to 94 ppm). Although most deposits in the Moa Bay lateritic district are classified as oxide type, Yamanigüey (avg Ni grade of 1.98%) is characterized by well-developed saprolite horizons, with secondary serpentine (serpentine II) and garnierite being the main Ni-bearing phases. |
| publishDate |
2024 |
| dc.date.none.fl_str_mv |
2024 |
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info:eu-repo/semantics/article info:eu-repo/semantics/acceptedVersion |
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article |
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acceptedVersion |
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https://hdl.handle.net/2445/227510 |
| url |
https://hdl.handle.net/2445/227510 |
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Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
Versió postprint del document publicat a: https://doi.org/10.5382/econgeo.5101 Economic Geology, 2024, vol. 119, num.7, p. 1685-1706 https://doi.org/10.5382/econgeo.5101 |
| dc.rights.none.fl_str_mv |
(c) Society of Economic Geologists, 2024 info:eu-repo/semantics/openAccess |
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(c) Society of Economic Geologists, 2024 |
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openAccess |
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application/pdf |
| dc.publisher.none.fl_str_mv |
Society of Economic Geologists |
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Society of Economic Geologists |
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Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada) reponame:Dipòsit Digital de la UB instname:Universidad de Barcelona |
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Universidad de Barcelona |
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Dipòsit Digital de la UB |
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Dipòsit Digital de la UB |
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15.811543 |