Mineralogical zoning with X-ray difraction for the optimization of metallurgical treatment in the Toromocho Deposit

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The Toromocho Deposit is a Porphyry Skarn deposit with an extension of 5 km by 6 km, geologically it is made up of volcanic rocks from Mitú and limestone from Pucara and tertiary intrusives. The mineralization is mainly due to veins that cross the entire Morococha district from East to West, which a...

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Detalles Bibliográficos
Autores: Flores Barrón, Ronald Eugenio, Guadalupe Gómez, Enrique
Formato: artículo
Fecha de Publicación:2020
Institución:Universidad Nacional Mayor de San Marcos
Repositorio:Revistas - Universidad Nacional Mayor de San Marcos
Lenguaje:español
OAI Identifier:oai:ojs.csi.unmsm:article/19188
Enlace del recurso:https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/19188
Nivel de acceso:acceso abierto
Materia:Porphyry
mineralization
veins
mantles
stock work
blending
Pórfido
mineralización
vetas
mantos
stockwork
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oai_identifier_str oai:ojs.csi.unmsm:article/19188
network_acronym_str REVUNMSM
network_name_str Revistas - Universidad Nacional Mayor de San Marcos
repository_id_str
dc.title.none.fl_str_mv Mineralogical zoning with X-ray difraction for the optimization of metallurgical treatment in the Toromocho Deposit
Zonamiento mineralógico con difracción de rayos X para la optimización del tratamiento metalúrgico en el Yacimiento Toromocho
title Mineralogical zoning with X-ray difraction for the optimization of metallurgical treatment in the Toromocho Deposit
spellingShingle Mineralogical zoning with X-ray difraction for the optimization of metallurgical treatment in the Toromocho Deposit
Flores Barrón, Ronald Eugenio
Porphyry
mineralization
veins
mantles
stock work
blending
Pórfido
mineralización
vetas
mantos
stockwork
blending
title_short Mineralogical zoning with X-ray difraction for the optimization of metallurgical treatment in the Toromocho Deposit
title_full Mineralogical zoning with X-ray difraction for the optimization of metallurgical treatment in the Toromocho Deposit
title_fullStr Mineralogical zoning with X-ray difraction for the optimization of metallurgical treatment in the Toromocho Deposit
title_full_unstemmed Mineralogical zoning with X-ray difraction for the optimization of metallurgical treatment in the Toromocho Deposit
title_sort Mineralogical zoning with X-ray difraction for the optimization of metallurgical treatment in the Toromocho Deposit
dc.creator.none.fl_str_mv Flores Barrón, Ronald Eugenio
Guadalupe Gómez, Enrique
author Flores Barrón, Ronald Eugenio
author_facet Flores Barrón, Ronald Eugenio
Guadalupe Gómez, Enrique
author_role author
author2 Guadalupe Gómez, Enrique
author2_role author
dc.subject.none.fl_str_mv Porphyry
mineralization
veins
mantles
stock work
blending
Pórfido
mineralización
vetas
mantos
stockwork
blending
topic Porphyry
mineralization
veins
mantles
stock work
blending
Pórfido
mineralización
vetas
mantos
stockwork
blending
description The Toromocho Deposit is a Porphyry Skarn deposit with an extension of 5 km by 6 km, geologically it is made up of volcanic rocks from Mitú and limestone from Pucara and tertiary intrusives. The mineralization is mainly due to veins that cross the entire Morococha district from East to West, which are filled with Pb, Zn and Ag Zinc mantles minerals located in the limestones and in a disseminated form, also located in the limestones and in the Volcanic-limestone-intrusive contacts and also scattered pyritic bodies with copper mineralization. Regarding its mineralization, it is very complex finding veins, mantles, stock work, scattered bodies, finding minerals that greatly affect metallurgical treatment such as arsenic. The results of the XRD studies allow us to characterize the existing minerals in the deposit, from the contaminating minerals to be able to perform a good blending, control talc, fluorine, magnesium, zinc, etc. The higher the talc content in CMC, the more effective it is with naturally buoyant bargains to achieve a minimum degree of 20%. It requires 700g / l of CMC. According to agreement with the metallurgy, planning and geology area, we came to terms of not considering some penalizable minerals such as fluorine, because in the central part of the deposit there is high fluorine as well as a high degree of copper, which allows blending. to be able to raise the copper grade, but in the metallurgical plant the molybdenum plant process has to be activated to be able to clean the mineral with high fluorine and talc with the addition of NaSH.
publishDate 2020
dc.date.none.fl_str_mv 2020-11-30
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/19188
10.15381/iigeo.v23i46.19188
url https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/19188
identifier_str_mv 10.15381/iigeo.v23i46.19188
dc.language.none.fl_str_mv spa
language spa
dc.relation.none.fl_str_mv https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/19188/16091
dc.rights.none.fl_str_mv Derechos de autor 2020 Ronald Eugenio Flores Barrón, Enrique Guadalupe Gómez
https://creativecommons.org/licenses/by-nc-sa/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Derechos de autor 2020 Ronald Eugenio Flores Barrón, Enrique Guadalupe Gómez
https://creativecommons.org/licenses/by-nc-sa/4.0
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidad Nacional Mayor de San Marcos, Facultad de Ingeniería Geológica, Minera, Metalúrgica y Geográfica
publisher.none.fl_str_mv Universidad Nacional Mayor de San Marcos, Facultad de Ingeniería Geológica, Minera, Metalúrgica y Geográfica
dc.source.none.fl_str_mv Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 23 No. 46 (2020); 121-129
Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 23 Núm. 46 (2020); 121-129
1682-3087
1561-0888
reponame:Revistas - Universidad Nacional Mayor de San Marcos
instname:Universidad Nacional Mayor de San Marcos
instacron:UNMSM
instname_str Universidad Nacional Mayor de San Marcos
instacron_str UNMSM
institution UNMSM
reponame_str Revistas - Universidad Nacional Mayor de San Marcos
collection Revistas - Universidad Nacional Mayor de San Marcos
repository.name.fl_str_mv
repository.mail.fl_str_mv
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spelling Mineralogical zoning with X-ray difraction for the optimization of metallurgical treatment in the Toromocho DepositZonamiento mineralógico con difracción de rayos X para la optimización del tratamiento metalúrgico en el Yacimiento ToromochoFlores Barrón, Ronald EugenioGuadalupe Gómez, EnriquePorphyrymineralizationveinsmantlesstock workblendingPórfidomineralizaciónvetasmantosstockworkblendingThe Toromocho Deposit is a Porphyry Skarn deposit with an extension of 5 km by 6 km, geologically it is made up of volcanic rocks from Mitú and limestone from Pucara and tertiary intrusives. The mineralization is mainly due to veins that cross the entire Morococha district from East to West, which are filled with Pb, Zn and Ag Zinc mantles minerals located in the limestones and in a disseminated form, also located in the limestones and in the Volcanic-limestone-intrusive contacts and also scattered pyritic bodies with copper mineralization. Regarding its mineralization, it is very complex finding veins, mantles, stock work, scattered bodies, finding minerals that greatly affect metallurgical treatment such as arsenic. The results of the XRD studies allow us to characterize the existing minerals in the deposit, from the contaminating minerals to be able to perform a good blending, control talc, fluorine, magnesium, zinc, etc. The higher the talc content in CMC, the more effective it is with naturally buoyant bargains to achieve a minimum degree of 20%. It requires 700g / l of CMC. According to agreement with the metallurgy, planning and geology area, we came to terms of not considering some penalizable minerals such as fluorine, because in the central part of the deposit there is high fluorine as well as a high degree of copper, which allows blending. to be able to raise the copper grade, but in the metallurgical plant the molybdenum plant process has to be activated to be able to clean the mineral with high fluorine and talc with the addition of NaSH.El yacimiento Toromocho es un yacimiento pórfido skarn con una extensión de 5 km por 6 km, geológicamente está constituida por rocas volcánicas del Mitu y calizas del Pucara e intrusivos terciario. La mineralización, mayormente está dada por vetas que atraviesan de Este a Oeste en todo Morococha que están rellenadas con minerales de Pb, Zn y Ag mantos de Zinc emplazados en las calizas y en forma diseminada, también emplazados en las calizas y en los contactos volcánicos–caliza-intrusivo y también cuerpos piritosos diseminados con mineralización de cobre. En cuanto a su mineralización es muy compleja encontrando mantos, vetas, stockwork, diseminado cuerpos encontrando minerales que afectan mucho el tratamiento metalúrgico como es el arsénico. Los resultados de los estudios de XRD nos permite caracterizar los minerales existentes en el yacimiento, de los minerales contaminantes para poder realizar un buen blending, controlar el talco, fluor magnesio, zinc, etc. A mayor contenido de talco en CMC es más efectivo a un con gangas naturalmente flotables para lograr un grado mínimo de 20% requiere 700g/l de CMC. Según acuerdo con el área de metalurgia, planeamiento y geología se llegaron a nos términos de no considerar algunos minerales penalizables como es el fluor, porque en la parte central del yacimiento se tiene alto fluor como también alto grado de cobre que esto permite realizar un blending para poder levantar la ley de cobre, pero en la planta metalúrgica se tiene que activar el proceso de la planta de molibdeno para poder limpiar el mineral con alto fluor y talco con la adición del NaSH.Universidad Nacional Mayor de San Marcos, Facultad de Ingeniería Geológica, Minera, Metalúrgica y Geográfica2020-11-30info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/1918810.15381/iigeo.v23i46.19188Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 23 No. 46 (2020); 121-129Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 23 Núm. 46 (2020); 121-1291682-30871561-0888reponame:Revistas - Universidad Nacional Mayor de San Marcosinstname:Universidad Nacional Mayor de San Marcosinstacron:UNMSMspahttps://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/19188/16091Derechos de autor 2020 Ronald Eugenio Flores Barrón, Enrique Guadalupe Gómezhttps://creativecommons.org/licenses/by-nc-sa/4.0info:eu-repo/semantics/openAccessoai:ojs.csi.unmsm:article/191882020-11-30T13:52:39Z
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