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Early crustal processes revealed by the ejection site of the oldest martian meteorite
The formation and differentiation of the crust of Mars in the first tens of millions of years after its accretion can only be deciphered from incredibly limited records. The martian breccia NWA 7034 and its paired stones is one of them. This meteorite contains the oldest martian igneous material eve...
Autores principales: | , , , , , , , , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2022
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9276826/ https://www.ncbi.nlm.nih.gov/pubmed/35821210 http://dx.doi.org/10.1038/s41467-022-31444-8 |
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author | Lagain, A. Bouley, S. Zanda, B. Miljković, K. Rajšić, A. Baratoux, D. Payré, V. Doucet, L. S. Timms, N. E. Hewins, R. Benedix, G. K. Malarewic, V. Servis, K. Bland, P. A. |
author_facet | Lagain, A. Bouley, S. Zanda, B. Miljković, K. Rajšić, A. Baratoux, D. Payré, V. Doucet, L. S. Timms, N. E. Hewins, R. Benedix, G. K. Malarewic, V. Servis, K. Bland, P. A. |
author_sort | Lagain, A. |
collection | PubMed |
description | The formation and differentiation of the crust of Mars in the first tens of millions of years after its accretion can only be deciphered from incredibly limited records. The martian breccia NWA 7034 and its paired stones is one of them. This meteorite contains the oldest martian igneous material ever dated: ~4.5 Ga old. However, its source and geological context have so far remained unknown. Here, we show that the meteorite was ejected 5–10 Ma ago from the north-east of the Terra Cimmeria—Sirenum province, in the southern hemisphere of Mars. More specifically, the breccia belongs to the ejecta deposits of the Khujirt crater formed 1.5 Ga ago, and it was ejected as a result of the formation of the Karratha crater 5–10 Ma ago. Our findings demonstrate that the Terra Cimmeria—Sirenum province is a relic of the differentiated primordial martian crust, formed shortly after the accretion of the planet, and that it constitutes a unique record of early crustal processes. This province is an ideal landing site for future missions aiming to unravel the first tens of millions of years of the history of Mars and, by extension, of all terrestrial planets, including the Earth. |
format | Online Article Text |
id | pubmed-9276826 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2022 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-92768262022-07-14 Early crustal processes revealed by the ejection site of the oldest martian meteorite Lagain, A. Bouley, S. Zanda, B. Miljković, K. Rajšić, A. Baratoux, D. Payré, V. Doucet, L. S. Timms, N. E. Hewins, R. Benedix, G. K. Malarewic, V. Servis, K. Bland, P. A. Nat Commun Article The formation and differentiation of the crust of Mars in the first tens of millions of years after its accretion can only be deciphered from incredibly limited records. The martian breccia NWA 7034 and its paired stones is one of them. This meteorite contains the oldest martian igneous material ever dated: ~4.5 Ga old. However, its source and geological context have so far remained unknown. Here, we show that the meteorite was ejected 5–10 Ma ago from the north-east of the Terra Cimmeria—Sirenum province, in the southern hemisphere of Mars. More specifically, the breccia belongs to the ejecta deposits of the Khujirt crater formed 1.5 Ga ago, and it was ejected as a result of the formation of the Karratha crater 5–10 Ma ago. Our findings demonstrate that the Terra Cimmeria—Sirenum province is a relic of the differentiated primordial martian crust, formed shortly after the accretion of the planet, and that it constitutes a unique record of early crustal processes. This province is an ideal landing site for future missions aiming to unravel the first tens of millions of years of the history of Mars and, by extension, of all terrestrial planets, including the Earth. Nature Publishing Group UK 2022-07-12 /pmc/articles/PMC9276826/ /pubmed/35821210 http://dx.doi.org/10.1038/s41467-022-31444-8 Text en © The Author(s) 2022 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . |
spellingShingle | Article Lagain, A. Bouley, S. Zanda, B. Miljković, K. Rajšić, A. Baratoux, D. Payré, V. Doucet, L. S. Timms, N. E. Hewins, R. Benedix, G. K. Malarewic, V. Servis, K. Bland, P. A. Early crustal processes revealed by the ejection site of the oldest martian meteorite |
title | Early crustal processes revealed by the ejection site of the oldest martian meteorite |
title_full | Early crustal processes revealed by the ejection site of the oldest martian meteorite |
title_fullStr | Early crustal processes revealed by the ejection site of the oldest martian meteorite |
title_full_unstemmed | Early crustal processes revealed by the ejection site of the oldest martian meteorite |
title_short | Early crustal processes revealed by the ejection site of the oldest martian meteorite |
title_sort | early crustal processes revealed by the ejection site of the oldest martian meteorite |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9276826/ https://www.ncbi.nlm.nih.gov/pubmed/35821210 http://dx.doi.org/10.1038/s41467-022-31444-8 |
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