The Fe and Zn isotope composition of deep mantle source regions: Insights from Baffin Island picrites
Young (61 Ma) unaltered picrites from Baffin Island, northwest Canada, possess some of the highest 3He/4He (up to 50 Ra) seen on Earth, and provide a unique opportunity to study primordial mantle that has escaped subsequent chemical modification. These high-degree partial melts also record anomalous...
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ftunivcam:oai:www.repository.cam.ac.uk:1810/280611 2024-01-14T10:05:35+01:00 The Fe and Zn isotope composition of deep mantle source regions: Insights from Baffin Island picrites McCoy-West, AJ Fitton, JG Pons, ML Inglis, EC Williams, HM 2018 application/pdf https://www.repository.cam.ac.uk/handle/1810/280611 https://doi.org/10.17863/CAM.27977 eng eng Elsevier BV http://dx.doi.org/10.1016/j.gca.2018.07.021 Geochimica et Cosmochimica Acta https://www.repository.cam.ac.uk/handle/1810/280611 doi:10.17863/CAM.27977 Attribution-NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/licenses/by-nc-nd/4.0/ Iron Zinc Stable isotopes Picrites Komatiites Olivine Sulfide Article 2018 ftunivcam https://doi.org/10.17863/CAM.27977 2023-12-21T23:24:28Z Young (61 Ma) unaltered picrites from Baffin Island, northwest Canada, possess some of the highest 3He/4He (up to 50 Ra) seen on Earth, and provide a unique opportunity to study primordial mantle that has escaped subsequent chemical modification. These high-degree partial melts also record anomalously high 182W/184W ratios, but their Sr-Nd-Hf-Pb isotopic compositons (including 142Nd) are indistinguishable from those of North Atlantic mid-ocean ridge basalts. New high precision Fe and Zn stable isotope analyses of Baffin Island picrites show limited variability with δ56Fe ranging from −0.03‰ to 0.13‰ and δ66Zn varying from 0.18‰ to 0.28‰. However, a clear inflection is seen in both sets of isotope data around the composition of the parental melt (MgO = 21 wt %; δ56Fe = 0.08 ± 0.04‰; and δ66Zn = 0.24 ± 0.03‰), with two diverging trends interpreted to reflect the crystallisation of olivine and spinel in low-MgO samples and the accumulation of olivine at higher MgO. Olivine mineral separates are significantly isotopically lighter than their corresponding whole rocks (δ56Fe ≥ −0.62‰ and δ66Zn ≥ −0.22‰), with analyses of individual olivine phenocrysts having extremely variable Fe isotope compositions (δ56Fe = −0.01‰ to −0.80‰). By carrying out modelling in three-isotope space, we show that the very negative Fe isotope compositions of olivine phenocryst are the result of kinetic isotope fractionation from disequilibrium diffusional processes. An excellent correlation is observed between δ56Fe and δ66Zn, demonstrating that Zn isotopes are fractionated by the same processes as Fe in simple systems dominated by magmatic olivine. The incompatible behaviour of Cu during magmatic evolution is consistent with the sulfide- undersaturated nature of these melts. Consequently Zn behaves as a purely lithophile element, and estimates of the bulk Earth Zn isotope composition based on Baffin Island should therefore be robust. The ancient undegassed lower mantle sampled at Baffin Island possesses a δ56Fe value that is within error of ... Article in Journal/Newspaper Baffin Island Baffin North Atlantic Apollo - University of Cambridge Repository Baffin Island Canada |
institution |
Open Polar |
collection |
Apollo - University of Cambridge Repository |
op_collection_id |
ftunivcam |
language |
English |
topic |
Iron Zinc Stable isotopes Picrites Komatiites Olivine Sulfide |
spellingShingle |
Iron Zinc Stable isotopes Picrites Komatiites Olivine Sulfide McCoy-West, AJ Fitton, JG Pons, ML Inglis, EC Williams, HM The Fe and Zn isotope composition of deep mantle source regions: Insights from Baffin Island picrites |
topic_facet |
Iron Zinc Stable isotopes Picrites Komatiites Olivine Sulfide |
description |
Young (61 Ma) unaltered picrites from Baffin Island, northwest Canada, possess some of the highest 3He/4He (up to 50 Ra) seen on Earth, and provide a unique opportunity to study primordial mantle that has escaped subsequent chemical modification. These high-degree partial melts also record anomalously high 182W/184W ratios, but their Sr-Nd-Hf-Pb isotopic compositons (including 142Nd) are indistinguishable from those of North Atlantic mid-ocean ridge basalts. New high precision Fe and Zn stable isotope analyses of Baffin Island picrites show limited variability with δ56Fe ranging from −0.03‰ to 0.13‰ and δ66Zn varying from 0.18‰ to 0.28‰. However, a clear inflection is seen in both sets of isotope data around the composition of the parental melt (MgO = 21 wt %; δ56Fe = 0.08 ± 0.04‰; and δ66Zn = 0.24 ± 0.03‰), with two diverging trends interpreted to reflect the crystallisation of olivine and spinel in low-MgO samples and the accumulation of olivine at higher MgO. Olivine mineral separates are significantly isotopically lighter than their corresponding whole rocks (δ56Fe ≥ −0.62‰ and δ66Zn ≥ −0.22‰), with analyses of individual olivine phenocrysts having extremely variable Fe isotope compositions (δ56Fe = −0.01‰ to −0.80‰). By carrying out modelling in three-isotope space, we show that the very negative Fe isotope compositions of olivine phenocryst are the result of kinetic isotope fractionation from disequilibrium diffusional processes. An excellent correlation is observed between δ56Fe and δ66Zn, demonstrating that Zn isotopes are fractionated by the same processes as Fe in simple systems dominated by magmatic olivine. The incompatible behaviour of Cu during magmatic evolution is consistent with the sulfide- undersaturated nature of these melts. Consequently Zn behaves as a purely lithophile element, and estimates of the bulk Earth Zn isotope composition based on Baffin Island should therefore be robust. The ancient undegassed lower mantle sampled at Baffin Island possesses a δ56Fe value that is within error of ... |
format |
Article in Journal/Newspaper |
author |
McCoy-West, AJ Fitton, JG Pons, ML Inglis, EC Williams, HM |
author_facet |
McCoy-West, AJ Fitton, JG Pons, ML Inglis, EC Williams, HM |
author_sort |
McCoy-West, AJ |
title |
The Fe and Zn isotope composition of deep mantle source regions: Insights from Baffin Island picrites |
title_short |
The Fe and Zn isotope composition of deep mantle source regions: Insights from Baffin Island picrites |
title_full |
The Fe and Zn isotope composition of deep mantle source regions: Insights from Baffin Island picrites |
title_fullStr |
The Fe and Zn isotope composition of deep mantle source regions: Insights from Baffin Island picrites |
title_full_unstemmed |
The Fe and Zn isotope composition of deep mantle source regions: Insights from Baffin Island picrites |
title_sort |
fe and zn isotope composition of deep mantle source regions: insights from baffin island picrites |
publisher |
Elsevier BV |
publishDate |
2018 |
url |
https://www.repository.cam.ac.uk/handle/1810/280611 https://doi.org/10.17863/CAM.27977 |
geographic |
Baffin Island Canada |
geographic_facet |
Baffin Island Canada |
genre |
Baffin Island Baffin North Atlantic |
genre_facet |
Baffin Island Baffin North Atlantic |
op_relation |
https://www.repository.cam.ac.uk/handle/1810/280611 doi:10.17863/CAM.27977 |
op_rights |
Attribution-NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/licenses/by-nc-nd/4.0/ |
op_doi |
https://doi.org/10.17863/CAM.27977 |
_version_ |
1788059933808263168 |