Mercury isotopic composition of various ocean island basalts

The mercury isotopic composition of the basalts was measured in 2021 by MC-ICPMS, using a Nu Plasma Instrument. We report both mass-dependent ( δ202Hg) and mass-independent (Δ199Hg, Δ201Hg) isotopic composition of mercury. The mantle composition least affected by crustal recycling is estimated from...

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Main Author: Moynier, Frederic
Format: Dataset
Language:unknown
Published: Mendeley 2021
Subjects:
Online Access:https://dx.doi.org/10.17632/fyxkjrpnhh.1
https://data.mendeley.com/datasets/fyxkjrpnhh/1
id ftdatacite:10.17632/fyxkjrpnhh.1
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spelling ftdatacite:10.17632/fyxkjrpnhh.1 2023-05-15T16:48:27+02:00 Mercury isotopic composition of various ocean island basalts Moynier, Frederic 2021 https://dx.doi.org/10.17632/fyxkjrpnhh.1 https://data.mendeley.com/datasets/fyxkjrpnhh/1 unknown Mendeley https://dx.doi.org/10.17632/fyxkjrpnhh Creative Commons Attribution 4.0 International info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Geochemistry FOS Earth and related environmental sciences dataset Dataset 2021 ftdatacite https://doi.org/10.17632/fyxkjrpnhh.1 https://doi.org/10.17632/fyxkjrpnhh 2021-11-05T12:55:41Z The mercury isotopic composition of the basalts was measured in 2021 by MC-ICPMS, using a Nu Plasma Instrument. We report both mass-dependent ( δ202Hg) and mass-independent (Δ199Hg, Δ201Hg) isotopic composition of mercury. The mantle composition least affected by crustal recycling is estimated from high-3He/4He lavas from Samoa and Iceland, providing an average of Δ199Hg=0.000.10, Δ201Hg=-0.020.0.09, δ202Hg=-1.71.2; 2SD, N=11. HIMU-type lava shows positive Δ199Hg, consistent with the incorporation of altered oceanic crust in its mantle source, while a Samoan (EM2) lava has negative Δ199Hg reflecting incorporation of continental crust materials into its source. Dataset Iceland Ocean Island DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Geochemistry
FOS Earth and related environmental sciences
spellingShingle Geochemistry
FOS Earth and related environmental sciences
Moynier, Frederic
Mercury isotopic composition of various ocean island basalts
topic_facet Geochemistry
FOS Earth and related environmental sciences
description The mercury isotopic composition of the basalts was measured in 2021 by MC-ICPMS, using a Nu Plasma Instrument. We report both mass-dependent ( δ202Hg) and mass-independent (Δ199Hg, Δ201Hg) isotopic composition of mercury. The mantle composition least affected by crustal recycling is estimated from high-3He/4He lavas from Samoa and Iceland, providing an average of Δ199Hg=0.000.10, Δ201Hg=-0.020.0.09, δ202Hg=-1.71.2; 2SD, N=11. HIMU-type lava shows positive Δ199Hg, consistent with the incorporation of altered oceanic crust in its mantle source, while a Samoan (EM2) lava has negative Δ199Hg reflecting incorporation of continental crust materials into its source.
format Dataset
author Moynier, Frederic
author_facet Moynier, Frederic
author_sort Moynier, Frederic
title Mercury isotopic composition of various ocean island basalts
title_short Mercury isotopic composition of various ocean island basalts
title_full Mercury isotopic composition of various ocean island basalts
title_fullStr Mercury isotopic composition of various ocean island basalts
title_full_unstemmed Mercury isotopic composition of various ocean island basalts
title_sort mercury isotopic composition of various ocean island basalts
publisher Mendeley
publishDate 2021
url https://dx.doi.org/10.17632/fyxkjrpnhh.1
https://data.mendeley.com/datasets/fyxkjrpnhh/1
genre Iceland
Ocean Island
genre_facet Iceland
Ocean Island
op_relation https://dx.doi.org/10.17632/fyxkjrpnhh
op_rights Creative Commons Attribution 4.0 International
info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.17632/fyxkjrpnhh.1
https://doi.org/10.17632/fyxkjrpnhh
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