Formation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses
The Candelaria iron oxide-copper-gold deposit in Chile was formed by superimposed, episodic hydrothermal pulses with contrasting composition and temperature, according to micro-textural and compositional variations in actinolite, a common alteration mineral. Iron oxide-copper-gold deposits are a glo...
Published in: | Communications Earth & Environment |
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Springernature, England
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ftunivchile:oai:repositorio.uchile.cl:2250/186385 2023-05-15T17:46:44+02:00 Formation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses Real, Irene del Reich Morales, Martín Herbert Simon, Adam C. Deditius, Artur Barra Pantoja, Luis Fernando Rodríguez Mustafa, María A. Thompson, John F. H. Roberts, Malcolm P. 2021 application/pdf https://doi.org/10.1038/s43247-021-00265-w https://repositorio.uchile.cl/handle/2250/186385 en eng Springernature, England Communications Earth & Environment (2021) 2:192 doi:10.1038/s43247-021-00265-w https://repositorio.uchile.cl/handle/2250/186385 Attribution-NonCommercial-NoDerivs 3.0 United States http://creativecommons.org/licenses/by-nc-nd/3.0/us/ CC-BY-NC-ND Communications Earth & Environment Carajas mineral province O Stable-isotopes Au-ag deposit Apatite ioa Iocg deposit Northwest-territories Structural controls Sulfur isotopes Prominent hill Gawler craton Artículo de revista 2021 ftunivchile https://doi.org/10.1038/s43247-021-00265-w 2022-07-02T23:49:28Z The Candelaria iron oxide-copper-gold deposit in Chile was formed by superimposed, episodic hydrothermal pulses with contrasting composition and temperature, according to micro-textural and compositional variations in actinolite, a common alteration mineral. Iron oxide-copper-gold deposits are a globally important source of copper, gold and critical commodities. However, they possess a range of characteristics related to a variety of tectono-magmatic settings that make development of a general genetic model challenging. Here we investigate micro-textural and compositional variations in actinolite, to constrain the thermal evolution of the Candelaria iron oxide-copper-gold deposit in Chile. We identify at least two mineralization stages comprising an early 675-800 degrees C iron oxide-apatite type mineralization overprinted by a later copper-rich fluid at around 550-700 degrees C. We propose that these distinct stages were caused by episodic pulses of injection of magmatic-hydrothermal fluids from crystallizing magmas at depth. We suggest that the mineralisation stages we identify were the result of temperature gradients attributable to changes in the magmatic source, rather than variations in formation depth, and that actinolite chemistry can be used as a proxy for formation temperature in iron oxide-copper-gold systems. ANID through Millennium Science Initiative Program NCN13_065 Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT) CONICYT FONDECYT 3200532 ANID through FONDECYT grant 1190105 National Science Foundation (NSF) 1924142 Versión publicada - versión final del editor Article in Journal/Newspaper Northwest Territories Universidad de Chile: Repositorio académico Candelaria ENVELOPE(-63.750,-63.750,-66.167,-66.167) Northwest Territories Communications Earth & Environment 2 1 |
institution |
Open Polar |
collection |
Universidad de Chile: Repositorio académico |
op_collection_id |
ftunivchile |
language |
English |
topic |
Carajas mineral province O Stable-isotopes Au-ag deposit Apatite ioa Iocg deposit Northwest-territories Structural controls Sulfur isotopes Prominent hill Gawler craton |
spellingShingle |
Carajas mineral province O Stable-isotopes Au-ag deposit Apatite ioa Iocg deposit Northwest-territories Structural controls Sulfur isotopes Prominent hill Gawler craton Real, Irene del Reich Morales, Martín Herbert Simon, Adam C. Deditius, Artur Barra Pantoja, Luis Fernando Rodríguez Mustafa, María A. Thompson, John F. H. Roberts, Malcolm P. Formation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses |
topic_facet |
Carajas mineral province O Stable-isotopes Au-ag deposit Apatite ioa Iocg deposit Northwest-territories Structural controls Sulfur isotopes Prominent hill Gawler craton |
description |
The Candelaria iron oxide-copper-gold deposit in Chile was formed by superimposed, episodic hydrothermal pulses with contrasting composition and temperature, according to micro-textural and compositional variations in actinolite, a common alteration mineral. Iron oxide-copper-gold deposits are a globally important source of copper, gold and critical commodities. However, they possess a range of characteristics related to a variety of tectono-magmatic settings that make development of a general genetic model challenging. Here we investigate micro-textural and compositional variations in actinolite, to constrain the thermal evolution of the Candelaria iron oxide-copper-gold deposit in Chile. We identify at least two mineralization stages comprising an early 675-800 degrees C iron oxide-apatite type mineralization overprinted by a later copper-rich fluid at around 550-700 degrees C. We propose that these distinct stages were caused by episodic pulses of injection of magmatic-hydrothermal fluids from crystallizing magmas at depth. We suggest that the mineralisation stages we identify were the result of temperature gradients attributable to changes in the magmatic source, rather than variations in formation depth, and that actinolite chemistry can be used as a proxy for formation temperature in iron oxide-copper-gold systems. ANID through Millennium Science Initiative Program NCN13_065 Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT) CONICYT FONDECYT 3200532 ANID through FONDECYT grant 1190105 National Science Foundation (NSF) 1924142 Versión publicada - versión final del editor |
format |
Article in Journal/Newspaper |
author |
Real, Irene del Reich Morales, Martín Herbert Simon, Adam C. Deditius, Artur Barra Pantoja, Luis Fernando Rodríguez Mustafa, María A. Thompson, John F. H. Roberts, Malcolm P. |
author_facet |
Real, Irene del Reich Morales, Martín Herbert Simon, Adam C. Deditius, Artur Barra Pantoja, Luis Fernando Rodríguez Mustafa, María A. Thompson, John F. H. Roberts, Malcolm P. |
author_sort |
Real, Irene del |
title |
Formation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses |
title_short |
Formation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses |
title_full |
Formation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses |
title_fullStr |
Formation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses |
title_full_unstemmed |
Formation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses |
title_sort |
formation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses |
publisher |
Springernature, England |
publishDate |
2021 |
url |
https://doi.org/10.1038/s43247-021-00265-w https://repositorio.uchile.cl/handle/2250/186385 |
long_lat |
ENVELOPE(-63.750,-63.750,-66.167,-66.167) |
geographic |
Candelaria Northwest Territories |
geographic_facet |
Candelaria Northwest Territories |
genre |
Northwest Territories |
genre_facet |
Northwest Territories |
op_source |
Communications Earth & Environment |
op_relation |
Communications Earth & Environment (2021) 2:192 doi:10.1038/s43247-021-00265-w https://repositorio.uchile.cl/handle/2250/186385 |
op_rights |
Attribution-NonCommercial-NoDerivs 3.0 United States http://creativecommons.org/licenses/by-nc-nd/3.0/us/ |
op_rightsnorm |
CC-BY-NC-ND |
op_doi |
https://doi.org/10.1038/s43247-021-00265-w |
container_title |
Communications Earth & Environment |
container_volume |
2 |
container_issue |
1 |
_version_ |
1766150560156745728 |