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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Deutsche Geologische Gesellschaft - Geologische Vereinigung e.V. (DGGV)
2023
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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) |
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DataCite Metadata Store (German National Library of Science and Technology) |
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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 |
genre_facet |
Iceland Ocean Island |
op_doi |
https://doi.org/10.48380/wffq-kj52 |
_version_ |
1789333755862712320 |