The ongoing homogenization of primordial and late-accreted components in ocean island basalt mantle sources ...

The formation of a segregated metallic core is viewed as an inevitable consequence of the growth of larger protoplanets. However, the effect of this process on the distribution of siderophile elements is hugely variable depending on the physiochemical nature of the protoplanet and the pressure and t...

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Main Authors: Peters, Bradley James, Mundl-Petermeier, Andrea, Finlayson, Valerie A.
Format: Text
Language:English
Published: Deutsche Geologische Gesellschaft - Geologische Vereinigung e.V. (DGGV) 2023
Subjects:
Online Access:https://dx.doi.org/10.48380/wffq-kj52
https://www.dggv.de/e-publikationen/the-ongoing-homogenization-of-primordial-and-late-accreted-components-in-ocean-island-basalt-mantle-sources
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spelling ftdatacite:10.48380/wffq-kj52 2024-01-28T10:06:42+01:00 The ongoing homogenization of primordial and late-accreted components in ocean island basalt mantle sources ... Peters, Bradley James Mundl-Petermeier, Andrea Finlayson, Valerie A. 2023 https://dx.doi.org/10.48380/wffq-kj52 https://www.dggv.de/e-publikationen/the-ongoing-homogenization-of-primordial-and-late-accreted-components-in-ocean-island-basalt-mantle-sources en eng Deutsche Geologische Gesellschaft - Geologische Vereinigung e.V. (DGGV) Abstract ScholaryArticle Text article-journal 2023 ftdatacite https://doi.org/10.48380/wffq-kj52 2024-01-04T23:34:38Z The formation of a segregated metallic core is viewed as an inevitable consequence of the growth of larger protoplanets. However, the effect of this process on the distribution of siderophile elements is hugely variable depending on the physiochemical nature of the protoplanet and the pressure and temperature at which metal-silicate equilibration occurs. On Earth, study of this process can be complicated by the overprinting effect of late accretion, which delivered additional siderophile element mass to the Earth. Along with Precambrian-aged mantle-derived rocks, ocean island basalts (OIB) are now recognized as an important source of information about the early siderophile evolution of the deep Earth. We demonstrate that the combined W isotopic and highly siderophile element (HSE) characteristics of major global hotspots (Hawaiʻi, Iceland, Réunion) preserve geochemical signatures secondary to Hadean metal-silicate equilibration that have not been overprinted by late accretion. Further, some OIB preserve ... Text Iceland Ocean Island DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
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op_collection_id ftdatacite
language English
description The formation of a segregated metallic core is viewed as an inevitable consequence of the growth of larger protoplanets. However, the effect of this process on the distribution of siderophile elements is hugely variable depending on the physiochemical nature of the protoplanet and the pressure and temperature at which metal-silicate equilibration occurs. On Earth, study of this process can be complicated by the overprinting effect of late accretion, which delivered additional siderophile element mass to the Earth. Along with Precambrian-aged mantle-derived rocks, ocean island basalts (OIB) are now recognized as an important source of information about the early siderophile evolution of the deep Earth. We demonstrate that the combined W isotopic and highly siderophile element (HSE) characteristics of major global hotspots (Hawaiʻi, Iceland, Réunion) preserve geochemical signatures secondary to Hadean metal-silicate equilibration that have not been overprinted by late accretion. Further, some OIB preserve ...
format Text
author Peters, Bradley James
Mundl-Petermeier, Andrea
Finlayson, Valerie A.
spellingShingle Peters, Bradley James
Mundl-Petermeier, Andrea
Finlayson, Valerie A.
The ongoing homogenization of primordial and late-accreted components in ocean island basalt mantle sources ...
author_facet Peters, Bradley James
Mundl-Petermeier, Andrea
Finlayson, Valerie A.
author_sort Peters, Bradley James
title The ongoing homogenization of primordial and late-accreted components in ocean island basalt mantle sources ...
title_short The ongoing homogenization of primordial and late-accreted components in ocean island basalt mantle sources ...
title_full The ongoing homogenization of primordial and late-accreted components in ocean island basalt mantle sources ...
title_fullStr The ongoing homogenization of primordial and late-accreted components in ocean island basalt mantle sources ...
title_full_unstemmed The ongoing homogenization of primordial and late-accreted components in ocean island basalt mantle sources ...
title_sort ongoing homogenization of primordial and late-accreted components in ocean island basalt mantle sources ...
publisher Deutsche Geologische Gesellschaft - Geologische Vereinigung e.V. (DGGV)
publishDate 2023
url https://dx.doi.org/10.48380/wffq-kj52
https://www.dggv.de/e-publikationen/the-ongoing-homogenization-of-primordial-and-late-accreted-components-in-ocean-island-basalt-mantle-sources
genre Iceland
Ocean Island
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Ocean Island
op_doi https://doi.org/10.48380/wffq-kj52
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