The manganese deposits of the Pampean Ranges, Argentina

The example of manganese mineralization studied in this paper makes up the major concentration of this element in Argentina. It comprises an area of 70 by 30 km in the eastern Sierras Pampeanas, located in Córdoba and Santiago del Estero provinces. It is quite unusual since it is hosted in granodior...

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Autores principales: Leal, P.R., Correa, M.J., Ametrano, S.J., Etcheverry, R.O., De Brodtkorb, M.K.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00084476_v46_n5_p1215_Leal
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spelling todo:paper_00084476_v46_n5_p1215_Leal2023-10-03T14:06:09Z The manganese deposits of the Pampean Ranges, Argentina Leal, P.R. Correa, M.J. Ametrano, S.J. Etcheverry, R.O. De Brodtkorb, M.K. Ambargasta Ranges Argentina Epithermal deposits Manganese Sierras Pampeanas Analytical geochemistry Barite Calcite Carbonate minerals Iron ores Manganese Manganese compounds Mineralogy Minerals Ores Oxide minerals Oxides Quartz Silica Ambargasta Ranges Aqueous solutions Argentina Chemical compositions Concentration of Continental environments Cryptomelane Electron micro probes Epithermal deposits Epithermal systems Gangue minerals Hollandite Hydrothermal fluids Isotopic analysis Last stages Low salinities Manganese oxides Meteoric waters Mineralization process Ore minerals Shear systems Sierras Pampeanas X- ray diffractions Manganese deposits chemical composition electron probe analysis epithermal deposit fluid inclusion granodiorite hydrothermal fluid isotopic analysis manganese deposit mineralization ore mineral X-ray diffraction Argentina Cordoba [Argentina] Santiago del Estero [Argentina] Sierras Pampeanas South America The example of manganese mineralization studied in this paper makes up the major concentration of this element in Argentina. It comprises an area of 70 by 30 km in the eastern Sierras Pampeanas, located in Córdoba and Santiago del Estero provinces. It is quite unusual since it is hosted in granodioritic and rhyodacitic rocks. Geochemical, petrological and structural analyses demonstrate that these rocks are unrelated to the mineralization process. The geometry and distribution of the veins are controlled by a dextral shear system related to north-south lineaments. Textural and structural analyses of the veins indicate four different stages of mineralization. Ore minerals precipitated during the first three, whereas the gangue was mainly formed during the last stage. X-ray diffraction and electron-microprobe studies show that Mn4+ oxides (hollandite, pyrolusite, ramsdellite, romanèchite and cryptomelane) associated with Fe3+ oxides (goethite and hematite) are the main ore minerals. Calcite, opal, barite, and lesser amounts of fluorite, quartz and "chalcedony" are the most common gangue minerals. Fluid-inclusion studies show that this mineralization was associated with aqueous solutions of low salinity and a temperature of about 125°C. Isotopic analyses based on several samples of calcite (δ13C, δ18O) and barite (δ 34S, δ18O) have demonstrated the dominance of meteoric waters in the hydrothermal fluids. Finally, the chemical composition of manganese oxides supports the hypothesis of an epithermal system developed in continental environments. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00084476_v46_n5_p1215_Leal
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Ambargasta Ranges
Argentina
Epithermal deposits
Manganese
Sierras Pampeanas
Analytical geochemistry
Barite
Calcite
Carbonate minerals
Iron ores
Manganese
Manganese compounds
Mineralogy
Minerals
Ores
Oxide minerals
Oxides
Quartz
Silica
Ambargasta Ranges
Aqueous solutions
Argentina
Chemical compositions
Concentration of
Continental environments
Cryptomelane
Electron micro probes
Epithermal deposits
Epithermal systems
Gangue minerals
Hollandite
Hydrothermal fluids
Isotopic analysis
Last stages
Low salinities
Manganese oxides
Meteoric waters
Mineralization process
Ore minerals
Shear systems
Sierras Pampeanas
X- ray diffractions
Manganese deposits
chemical composition
electron probe analysis
epithermal deposit
fluid inclusion
granodiorite
hydrothermal fluid
isotopic analysis
manganese deposit
mineralization
ore mineral
X-ray diffraction
Argentina
Cordoba [Argentina]
Santiago del Estero [Argentina]
Sierras Pampeanas
South America
spellingShingle Ambargasta Ranges
Argentina
Epithermal deposits
Manganese
Sierras Pampeanas
Analytical geochemistry
Barite
Calcite
Carbonate minerals
Iron ores
Manganese
Manganese compounds
Mineralogy
Minerals
Ores
Oxide minerals
Oxides
Quartz
Silica
Ambargasta Ranges
Aqueous solutions
Argentina
Chemical compositions
Concentration of
Continental environments
Cryptomelane
Electron micro probes
Epithermal deposits
Epithermal systems
Gangue minerals
Hollandite
Hydrothermal fluids
Isotopic analysis
Last stages
Low salinities
Manganese oxides
Meteoric waters
Mineralization process
Ore minerals
Shear systems
Sierras Pampeanas
X- ray diffractions
Manganese deposits
chemical composition
electron probe analysis
epithermal deposit
fluid inclusion
granodiorite
hydrothermal fluid
isotopic analysis
manganese deposit
mineralization
ore mineral
X-ray diffraction
Argentina
Cordoba [Argentina]
Santiago del Estero [Argentina]
Sierras Pampeanas
South America
Leal, P.R.
Correa, M.J.
Ametrano, S.J.
Etcheverry, R.O.
De Brodtkorb, M.K.
The manganese deposits of the Pampean Ranges, Argentina
topic_facet Ambargasta Ranges
Argentina
Epithermal deposits
Manganese
Sierras Pampeanas
Analytical geochemistry
Barite
Calcite
Carbonate minerals
Iron ores
Manganese
Manganese compounds
Mineralogy
Minerals
Ores
Oxide minerals
Oxides
Quartz
Silica
Ambargasta Ranges
Aqueous solutions
Argentina
Chemical compositions
Concentration of
Continental environments
Cryptomelane
Electron micro probes
Epithermal deposits
Epithermal systems
Gangue minerals
Hollandite
Hydrothermal fluids
Isotopic analysis
Last stages
Low salinities
Manganese oxides
Meteoric waters
Mineralization process
Ore minerals
Shear systems
Sierras Pampeanas
X- ray diffractions
Manganese deposits
chemical composition
electron probe analysis
epithermal deposit
fluid inclusion
granodiorite
hydrothermal fluid
isotopic analysis
manganese deposit
mineralization
ore mineral
X-ray diffraction
Argentina
Cordoba [Argentina]
Santiago del Estero [Argentina]
Sierras Pampeanas
South America
description The example of manganese mineralization studied in this paper makes up the major concentration of this element in Argentina. It comprises an area of 70 by 30 km in the eastern Sierras Pampeanas, located in Córdoba and Santiago del Estero provinces. It is quite unusual since it is hosted in granodioritic and rhyodacitic rocks. Geochemical, petrological and structural analyses demonstrate that these rocks are unrelated to the mineralization process. The geometry and distribution of the veins are controlled by a dextral shear system related to north-south lineaments. Textural and structural analyses of the veins indicate four different stages of mineralization. Ore minerals precipitated during the first three, whereas the gangue was mainly formed during the last stage. X-ray diffraction and electron-microprobe studies show that Mn4+ oxides (hollandite, pyrolusite, ramsdellite, romanèchite and cryptomelane) associated with Fe3+ oxides (goethite and hematite) are the main ore minerals. Calcite, opal, barite, and lesser amounts of fluorite, quartz and "chalcedony" are the most common gangue minerals. Fluid-inclusion studies show that this mineralization was associated with aqueous solutions of low salinity and a temperature of about 125°C. Isotopic analyses based on several samples of calcite (δ13C, δ18O) and barite (δ 34S, δ18O) have demonstrated the dominance of meteoric waters in the hydrothermal fluids. Finally, the chemical composition of manganese oxides supports the hypothesis of an epithermal system developed in continental environments.
format JOUR
author Leal, P.R.
Correa, M.J.
Ametrano, S.J.
Etcheverry, R.O.
De Brodtkorb, M.K.
author_facet Leal, P.R.
Correa, M.J.
Ametrano, S.J.
Etcheverry, R.O.
De Brodtkorb, M.K.
author_sort Leal, P.R.
title The manganese deposits of the Pampean Ranges, Argentina
title_short The manganese deposits of the Pampean Ranges, Argentina
title_full The manganese deposits of the Pampean Ranges, Argentina
title_fullStr The manganese deposits of the Pampean Ranges, Argentina
title_full_unstemmed The manganese deposits of the Pampean Ranges, Argentina
title_sort manganese deposits of the pampean ranges, argentina
url http://hdl.handle.net/20.500.12110/paper_00084476_v46_n5_p1215_Leal
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AT ametranosj themanganesedepositsofthepampeanrangesargentina
AT etcheverryro themanganesedepositsofthepampeanrangesargentina
AT debrodtkorbmk themanganesedepositsofthepampeanrangesargentina
AT lealpr manganesedepositsofthepampeanrangesargentina
AT correamj manganesedepositsofthepampeanrangesargentina
AT ametranosj manganesedepositsofthepampeanrangesargentina
AT etcheverryro manganesedepositsofthepampeanrangesargentina
AT debrodtkorbmk manganesedepositsofthepampeanrangesargentina
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