Thallium isotope data and major elements for Kamchatka arc lavas. Thallium isotope compositions of degassing experiments ...

Thallium (Tl) isotope ratios are an emerging tool that can be used to trace crustal recycling processes in arc lavas and ocean island basalts. Thallium is a highly volatile metal that is enriched in volcanic fumaroles, but it is unknown whether degassing of Tl from subaerial lavas has a significant...

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Main Author: Nielsen, Sune
Format: Dataset
Language:English
Published: Interdisciplinary Earth Data Alliance (IEDA) 2020
Subjects:
Online Access:https://dx.doi.org/10.26022/ieda/111790
https://ecl.earthchem.org/view.php?id=1790
id ftdatacite:10.26022/ieda/111790
record_format openpolar
spelling ftdatacite:10.26022/ieda/111790 2024-02-27T08:42:26+00:00 Thallium isotope data and major elements for Kamchatka arc lavas. Thallium isotope compositions of degassing experiments ... Nielsen, Sune 2020 application/vnd.ms-excel application/vnd.openxmlformats-officedocument.spreadsheetml.sheet https://dx.doi.org/10.26022/ieda/111790 https://ecl.earthchem.org/view.php?id=1790 en eng Interdisciplinary Earth Data Alliance (IEDA) Creative Commons Attribution Share Alike 4.0 International https://creativecommons.org/licenses/by-sa/4.0/legalcode cc-by-sa-4.0 Regional Continents, Oceans thallium isotopes, degassing experiments, volcanic rocks, Kamchatka arc dataset Collection Dataset 2020 ftdatacite https://doi.org/10.26022/ieda/111790 2024-02-01T15:06:42Z Thallium (Tl) isotope ratios are an emerging tool that can be used to trace crustal recycling processes in arc lavas and ocean island basalts. Thallium is a highly volatile metal that is enriched in volcanic fumaroles, but it is unknown whether degassing of Tl from subaerial lavas has a significant effect on their residual Tl isotope compositions. Here we present Tl isotope and concentration data from degassing experiments that are best explained by Rayleigh kinetic isotope fractionation during Tl loss. Our data closely follow predicted isotope fractionation models in which TlCl is the primary degassed species and where Tl diffusion in the gas phase is the main factor controlling the magnitude of isotope fractionation. We show that degassing into air should be associated with a net Tl isotope fractionation factor of net = 0.99967. We also show that lavas from three volcanoes in the Kamchatka arc exhibit Tl isotope and concentration patterns that closely follow the experimental results, implying that ... : Sune G. Nielsen, Yunchao Shu, Bernard J. Wood, Jerzy Blusztajn, Maureen Auro, C. Ashley Norris, Gerhard Wörner (2020) Thallium isotope fractionation during magma degassing: evidence from experiments and Kamchatka arc lavas, G-cubed ... Dataset Kamchatka 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 English
topic Regional Continents, Oceans
thallium isotopes, degassing experiments, volcanic rocks, Kamchatka arc
spellingShingle Regional Continents, Oceans
thallium isotopes, degassing experiments, volcanic rocks, Kamchatka arc
Nielsen, Sune
Thallium isotope data and major elements for Kamchatka arc lavas. Thallium isotope compositions of degassing experiments ...
topic_facet Regional Continents, Oceans
thallium isotopes, degassing experiments, volcanic rocks, Kamchatka arc
description Thallium (Tl) isotope ratios are an emerging tool that can be used to trace crustal recycling processes in arc lavas and ocean island basalts. Thallium is a highly volatile metal that is enriched in volcanic fumaroles, but it is unknown whether degassing of Tl from subaerial lavas has a significant effect on their residual Tl isotope compositions. Here we present Tl isotope and concentration data from degassing experiments that are best explained by Rayleigh kinetic isotope fractionation during Tl loss. Our data closely follow predicted isotope fractionation models in which TlCl is the primary degassed species and where Tl diffusion in the gas phase is the main factor controlling the magnitude of isotope fractionation. We show that degassing into air should be associated with a net Tl isotope fractionation factor of net = 0.99967. We also show that lavas from three volcanoes in the Kamchatka arc exhibit Tl isotope and concentration patterns that closely follow the experimental results, implying that ... : Sune G. Nielsen, Yunchao Shu, Bernard J. Wood, Jerzy Blusztajn, Maureen Auro, C. Ashley Norris, Gerhard Wörner (2020) Thallium isotope fractionation during magma degassing: evidence from experiments and Kamchatka arc lavas, G-cubed ...
format Dataset
author Nielsen, Sune
author_facet Nielsen, Sune
author_sort Nielsen, Sune
title Thallium isotope data and major elements for Kamchatka arc lavas. Thallium isotope compositions of degassing experiments ...
title_short Thallium isotope data and major elements for Kamchatka arc lavas. Thallium isotope compositions of degassing experiments ...
title_full Thallium isotope data and major elements for Kamchatka arc lavas. Thallium isotope compositions of degassing experiments ...
title_fullStr Thallium isotope data and major elements for Kamchatka arc lavas. Thallium isotope compositions of degassing experiments ...
title_full_unstemmed Thallium isotope data and major elements for Kamchatka arc lavas. Thallium isotope compositions of degassing experiments ...
title_sort thallium isotope data and major elements for kamchatka arc lavas. thallium isotope compositions of degassing experiments ...
publisher Interdisciplinary Earth Data Alliance (IEDA)
publishDate 2020
url https://dx.doi.org/10.26022/ieda/111790
https://ecl.earthchem.org/view.php?id=1790
genre Kamchatka
Ocean Island
genre_facet Kamchatka
Ocean Island
op_rights Creative Commons Attribution Share Alike 4.0 International
https://creativecommons.org/licenses/by-sa/4.0/legalcode
cc-by-sa-4.0
op_doi https://doi.org/10.26022/ieda/111790
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