The Älgliden Ni-Cu-Au deposit: magmatic sulfides in a subduction setting
International audience The origin of most major sulfide Ni-Cu deposits is attributed to the segregation of immiscible sulfide liquids from intraplate silicate melts, in response to assimilation of siliceous or sulfur-bearing rocks. The Älgliden gabbroic dike in the Skellefte district (Sweden) contai...
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ftinsu:oai:HAL:insu-03586614v1 2024-04-28T08:18:35+00:00 The Älgliden Ni-Cu-Au deposit: magmatic sulfides in a subduction setting Cordier, Carole Coin, Kevin Arndt, Nicholas T. Cartigny, Pierre Institut des Sciences de la Terre (ISTerre) Université Joseph Fourier - Grenoble 1 (UJF)-Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement IRD : UR219-PRES Université de Grenoble-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Institut de Physique du Globe de Paris (IPGP) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS) 2019 https://insu.hal.science/insu-03586614 https://doi.org/10.1007/s00126-019-00921-4 en eng HAL CCSD info:eu-repo/semantics/altIdentifier/doi/10.1007/s00126-019-00921-4 insu-03586614 https://insu.hal.science/insu-03586614 BIBCODE: 2019MinDe.55.1173C doi:10.1007/s00126-019-00921-4 Mineralium Deposita https://insu.hal.science/insu-03586614 Mineralium Deposita, 2019, 55, pp.1173-1196. ⟨10.1007/s00126-019-00921-4⟩ Skellefte district Ni-Cu ore deposit Arc magma Gold Melt reduction [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2019 ftinsu https://doi.org/10.1007/s00126-019-00921-4 2024-04-05T00:35:13Z International audience The origin of most major sulfide Ni-Cu deposits is attributed to the segregation of immiscible sulfide liquids from intraplate silicate melts, in response to assimilation of siliceous or sulfur-bearing rocks. The Älgliden gabbroic dike in the Skellefte district (Sweden) contains Ni-Cu sulfide mineralization that is atypical because it formed in an arc setting and has a high Au content and low Ni/Cu ratio. This association led previously to a model in which the mineralization was linked to the assimilation of Cu-Au porphyry wall rocks. Based on new petrological, geochemical, and S isotope analyses of the dike and its wall rocks, we propose that assimilation of mineralized wall rocks was not instrumental in the formation of the deposit. Instead, we propose that the sulfides segregated during olivine crystallization from an evolved arc basalt and were injected into the dike in an olivine-rich crystal mush. This scenario explains the uniform dissemination of sulfide ores within norites, together with the high Au content and low Ni/Cu ratio of the ores. We propose that sulfide segregation from oxidized arc basalt was triggered by a decrease in the oxidation state of the melt, likely due to the cooling of the silicate melt or to the interaction with meta-sediments rich in organic matter, as proposed for other arc-related Cu-Ni sulfide deposits in Fennoscandia and elsewhere. At Älgliden, melt reduction would have occurred relatively late during magma evolution, leading to the formation of an uneconomic deposit consisting of low Ni ores and lacking massive sulfides. Article in Journal/Newspaper Fennoscandia Institut national des sciences de l'Univers: HAL-INSU Mineralium Deposita 55 6 1173 1196 |
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Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
Skellefte district Ni-Cu ore deposit Arc magma Gold Melt reduction [SDU]Sciences of the Universe [physics] |
spellingShingle |
Skellefte district Ni-Cu ore deposit Arc magma Gold Melt reduction [SDU]Sciences of the Universe [physics] Cordier, Carole Coin, Kevin Arndt, Nicholas T. Cartigny, Pierre The Älgliden Ni-Cu-Au deposit: magmatic sulfides in a subduction setting |
topic_facet |
Skellefte district Ni-Cu ore deposit Arc magma Gold Melt reduction [SDU]Sciences of the Universe [physics] |
description |
International audience The origin of most major sulfide Ni-Cu deposits is attributed to the segregation of immiscible sulfide liquids from intraplate silicate melts, in response to assimilation of siliceous or sulfur-bearing rocks. The Älgliden gabbroic dike in the Skellefte district (Sweden) contains Ni-Cu sulfide mineralization that is atypical because it formed in an arc setting and has a high Au content and low Ni/Cu ratio. This association led previously to a model in which the mineralization was linked to the assimilation of Cu-Au porphyry wall rocks. Based on new petrological, geochemical, and S isotope analyses of the dike and its wall rocks, we propose that assimilation of mineralized wall rocks was not instrumental in the formation of the deposit. Instead, we propose that the sulfides segregated during olivine crystallization from an evolved arc basalt and were injected into the dike in an olivine-rich crystal mush. This scenario explains the uniform dissemination of sulfide ores within norites, together with the high Au content and low Ni/Cu ratio of the ores. We propose that sulfide segregation from oxidized arc basalt was triggered by a decrease in the oxidation state of the melt, likely due to the cooling of the silicate melt or to the interaction with meta-sediments rich in organic matter, as proposed for other arc-related Cu-Ni sulfide deposits in Fennoscandia and elsewhere. At Älgliden, melt reduction would have occurred relatively late during magma evolution, leading to the formation of an uneconomic deposit consisting of low Ni ores and lacking massive sulfides. |
author2 |
Institut des Sciences de la Terre (ISTerre) Université Joseph Fourier - Grenoble 1 (UJF)-Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement IRD : UR219-PRES Université de Grenoble-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Institut de Physique du Globe de Paris (IPGP) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Cordier, Carole Coin, Kevin Arndt, Nicholas T. Cartigny, Pierre |
author_facet |
Cordier, Carole Coin, Kevin Arndt, Nicholas T. Cartigny, Pierre |
author_sort |
Cordier, Carole |
title |
The Älgliden Ni-Cu-Au deposit: magmatic sulfides in a subduction setting |
title_short |
The Älgliden Ni-Cu-Au deposit: magmatic sulfides in a subduction setting |
title_full |
The Älgliden Ni-Cu-Au deposit: magmatic sulfides in a subduction setting |
title_fullStr |
The Älgliden Ni-Cu-Au deposit: magmatic sulfides in a subduction setting |
title_full_unstemmed |
The Älgliden Ni-Cu-Au deposit: magmatic sulfides in a subduction setting |
title_sort |
älgliden ni-cu-au deposit: magmatic sulfides in a subduction setting |
publisher |
HAL CCSD |
publishDate |
2019 |
url |
https://insu.hal.science/insu-03586614 https://doi.org/10.1007/s00126-019-00921-4 |
genre |
Fennoscandia |
genre_facet |
Fennoscandia |
op_source |
Mineralium Deposita https://insu.hal.science/insu-03586614 Mineralium Deposita, 2019, 55, pp.1173-1196. ⟨10.1007/s00126-019-00921-4⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1007/s00126-019-00921-4 insu-03586614 https://insu.hal.science/insu-03586614 BIBCODE: 2019MinDe.55.1173C doi:10.1007/s00126-019-00921-4 |
op_doi |
https://doi.org/10.1007/s00126-019-00921-4 |
container_title |
Mineralium Deposita |
container_volume |
55 |
container_issue |
6 |
container_start_page |
1173 |
op_container_end_page |
1196 |
_version_ |
1797582510413053952 |