Johnson et al. 2022. Giant impacts and the origin and evolution of continents. ...

Using the oxygen isotope compositions of dated magmatic zircon, we show that the Pilbara Craton in Western Australia, Earth’s best-preserved Archaean (4.0–2.5 billion years ago; Ga) continental remnant, was built in three stages. Stage 1 zircons (3.6–3.4 Ga) form two age clusters with one-third reco...

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Bibliographic Details
Main Authors: Johnson, Tim, Kirkland, Christopher, Lu, Yongjun, Smithies, Hugh, Brown, Michaeal, Hartnady, Michael
Format: Dataset
Language:English
Published: Interdisciplinary Earth Data Alliance (IEDA) 2022
Subjects:
Online Access:https://dx.doi.org/10.26022/ieda/112307
https://ecl.earthchem.org/view.php?id=2307
id ftdatacite:10.26022/ieda/112307
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spelling ftdatacite:10.26022/ieda/112307 2024-02-27T08:41:59+00:00 Johnson et al. 2022. Giant impacts and the origin and evolution of continents. ... Johnson, Tim Kirkland, Christopher Lu, Yongjun Smithies, Hugh Brown, Michaeal Hartnady, Michael 2022 application/vnd.openxmlformats-officedocument.spreadsheetml.sheet image/jpeg https://dx.doi.org/10.26022/ieda/112307 https://ecl.earthchem.org/view.php?id=2307 en eng Interdisciplinary Earth Data Alliance (IEDA) Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0] https://spdx.org/licenses/CC-BY-SA-4.0 Regional Continents, Oceans Archaean, early Earth, giant impacts, oxygen isotopes, Pilbara Craton dataset Collection Dataset 2022 ftdatacite https://doi.org/10.26022/ieda/112307 2024-02-01T15:06:42Z Using the oxygen isotope compositions of dated magmatic zircon, we show that the Pilbara Craton in Western Australia, Earth’s best-preserved Archaean (4.0–2.5 billion years ago; Ga) continental remnant, was built in three stages. Stage 1 zircons (3.6–3.4 Ga) form two age clusters with one-third recording sub-mantle δ18O, indicating crystallization from evolved magmas derived from hydrothermally-altered basaltic crust like that in modern-day Iceland. Stage 2 (3.4–3.0 Ga) zircons mostly have mantle-like δ18O and crystallized from parental magmas formed near the base of the evolving continental nucleus. Stage 3 (<3.0 Ga) zircons have above-mantle δ18O, indicating efficient recycling of supracrustal rocks. ... : Smithies, R. H., Lu, Y., Kirkland, C. L., Johnson, T. E., Champion, D. C., Mole D. R., Martin, L., Jeon, H., Wingate, M. T. D. & Johnson, S. P. (2021), Oxygen isotopes trace the origins of Earth’s earliest continental crust, Nature(592): 70–75. Johnson, T. E., Kirkland, C. L., Lu, Y., Smithies, R. H., Brown, M. & Hartnady, M. (2021), Giant impacts and the origin and evolution of continents, Nature(593): xxx–xxx. ... Dataset Iceland 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
Archaean, early Earth, giant impacts, oxygen isotopes, Pilbara Craton
spellingShingle Regional Continents, Oceans
Archaean, early Earth, giant impacts, oxygen isotopes, Pilbara Craton
Johnson, Tim
Kirkland, Christopher
Lu, Yongjun
Smithies, Hugh
Brown, Michaeal
Hartnady, Michael
Johnson et al. 2022. Giant impacts and the origin and evolution of continents. ...
topic_facet Regional Continents, Oceans
Archaean, early Earth, giant impacts, oxygen isotopes, Pilbara Craton
description Using the oxygen isotope compositions of dated magmatic zircon, we show that the Pilbara Craton in Western Australia, Earth’s best-preserved Archaean (4.0–2.5 billion years ago; Ga) continental remnant, was built in three stages. Stage 1 zircons (3.6–3.4 Ga) form two age clusters with one-third recording sub-mantle δ18O, indicating crystallization from evolved magmas derived from hydrothermally-altered basaltic crust like that in modern-day Iceland. Stage 2 (3.4–3.0 Ga) zircons mostly have mantle-like δ18O and crystallized from parental magmas formed near the base of the evolving continental nucleus. Stage 3 (<3.0 Ga) zircons have above-mantle δ18O, indicating efficient recycling of supracrustal rocks. ... : Smithies, R. H., Lu, Y., Kirkland, C. L., Johnson, T. E., Champion, D. C., Mole D. R., Martin, L., Jeon, H., Wingate, M. T. D. & Johnson, S. P. (2021), Oxygen isotopes trace the origins of Earth’s earliest continental crust, Nature(592): 70–75. Johnson, T. E., Kirkland, C. L., Lu, Y., Smithies, R. H., Brown, M. & Hartnady, M. (2021), Giant impacts and the origin and evolution of continents, Nature(593): xxx–xxx. ...
format Dataset
author Johnson, Tim
Kirkland, Christopher
Lu, Yongjun
Smithies, Hugh
Brown, Michaeal
Hartnady, Michael
author_facet Johnson, Tim
Kirkland, Christopher
Lu, Yongjun
Smithies, Hugh
Brown, Michaeal
Hartnady, Michael
author_sort Johnson, Tim
title Johnson et al. 2022. Giant impacts and the origin and evolution of continents. ...
title_short Johnson et al. 2022. Giant impacts and the origin and evolution of continents. ...
title_full Johnson et al. 2022. Giant impacts and the origin and evolution of continents. ...
title_fullStr Johnson et al. 2022. Giant impacts and the origin and evolution of continents. ...
title_full_unstemmed Johnson et al. 2022. Giant impacts and the origin and evolution of continents. ...
title_sort johnson et al. 2022. giant impacts and the origin and evolution of continents. ...
publisher Interdisciplinary Earth Data Alliance (IEDA)
publishDate 2022
url https://dx.doi.org/10.26022/ieda/112307
https://ecl.earthchem.org/view.php?id=2307
genre Iceland
genre_facet Iceland
op_rights Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
https://spdx.org/licenses/CC-BY-SA-4.0
op_doi https://doi.org/10.26022/ieda/112307
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