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.

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Autores principales:	Irene Del Real, Martin Reich, Adam C. Simon, Artur Deditius, Fernando Barra, María A. Rodríguez-Mustafa, John F. H. Thompson, Malcolm P. Roberts
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Geology QE1-996.5 Environmental sciences GE1-350
Acceso en línea:	https://doaj.org/article/aa348575608f40a39f1db814bac469aa
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spelling	oai:doaj.org-article:aa348575608f40a39f1db814bac469aa2021-12-02T17:23:39ZFormation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses10.1038/s43247-021-00265-w2662-4435https://doaj.org/article/aa348575608f40a39f1db814bac469aa2021-09-01T00:00:00Zhttps://doi.org/10.1038/s43247-021-00265-whttps://doaj.org/toc/2662-4435The 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.Irene Del RealMartin ReichAdam C. SimonArtur DeditiusFernando BarraMaría A. Rodríguez-MustafaJohn F. H. ThompsonMalcolm P. RobertsNature PortfolioarticleGeologyQE1-996.5Environmental sciencesGE1-350ENCommunications Earth & Environment, Vol 2, Iss 1, Pp 1-9 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Geology QE1-996.5 Environmental sciences GE1-350
spellingShingle	Geology QE1-996.5 Environmental sciences GE1-350 Irene Del Real Martin Reich Adam C. Simon Artur Deditius Fernando Barra María A. Rodríguez-Mustafa John F. H. Thompson Malcolm P. Roberts Formation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses
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.
format	article
author	Irene Del Real Martin Reich Adam C. Simon Artur Deditius Fernando Barra María A. Rodríguez-Mustafa John F. H. Thompson Malcolm P. Roberts
author_facet	Irene Del Real Martin Reich Adam C. Simon Artur Deditius Fernando Barra María A. Rodríguez-Mustafa John F. H. Thompson Malcolm P. Roberts
author_sort	Irene Del Real
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	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/aa348575608f40a39f1db814bac469aa
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Formation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses

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