The Tharsis mantle source of depleted shergottites revealed by 90 million impact craters

The ejection sites of the martian meteorites are still unknown. Here, the authors build a database of 90 million craters and show that Tharsis region is the most likely source of depleted shergottites ejected 1.1 Ma ago, thus confirming that some portions of the mantle were recently anomalously hot....

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Autores principales:	A. Lagain, G. K. Benedix, K. Servis, D. Baratoux, L. S. Doucet, A. Rajšic, H. A. R. Devillepoix, P. A. Bland, M. C. Towner, E. K. Sansom, K. Miljković
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/cb8a9e38289c4bd681296f17ff3947b5
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spelling	oai:doaj.org-article:cb8a9e38289c4bd681296f17ff3947b52021-11-08T11:11:41ZThe Tharsis mantle source of depleted shergottites revealed by 90 million impact craters10.1038/s41467-021-26648-32041-1723https://doaj.org/article/cb8a9e38289c4bd681296f17ff3947b52021-11-01T00:00:00Zhttps://doi.org/10.1038/s41467-021-26648-3https://doaj.org/toc/2041-1723The ejection sites of the martian meteorites are still unknown. Here, the authors build a database of 90 million craters and show that Tharsis region is the most likely source of depleted shergottites ejected 1.1 Ma ago, thus confirming that some portions of the mantle were recently anomalously hot.A. LagainG. K. BenedixK. ServisD. BaratouxL. S. DoucetA. RajšicH. A. R. DevillepoixP. A. BlandM. C. TownerE. K. SansomK. MiljkovićNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-9 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q A. Lagain G. K. Benedix K. Servis D. Baratoux L. S. Doucet A. Rajšic H. A. R. Devillepoix P. A. Bland M. C. Towner E. K. Sansom K. Miljković The Tharsis mantle source of depleted shergottites revealed by 90 million impact craters
description	The ejection sites of the martian meteorites are still unknown. Here, the authors build a database of 90 million craters and show that Tharsis region is the most likely source of depleted shergottites ejected 1.1 Ma ago, thus confirming that some portions of the mantle were recently anomalously hot.
format	article
author	A. Lagain G. K. Benedix K. Servis D. Baratoux L. S. Doucet A. Rajšic H. A. R. Devillepoix P. A. Bland M. C. Towner E. K. Sansom K. Miljković
author_facet	A. Lagain G. K. Benedix K. Servis D. Baratoux L. S. Doucet A. Rajšic H. A. R. Devillepoix P. A. Bland M. C. Towner E. K. Sansom K. Miljković
author_sort	A. Lagain
title	The Tharsis mantle source of depleted shergottites revealed by 90 million impact craters
title_short	The Tharsis mantle source of depleted shergottites revealed by 90 million impact craters
title_full	The Tharsis mantle source of depleted shergottites revealed by 90 million impact craters
title_fullStr	The Tharsis mantle source of depleted shergottites revealed by 90 million impact craters
title_full_unstemmed	The Tharsis mantle source of depleted shergottites revealed by 90 million impact craters
title_sort	tharsis mantle source of depleted shergottites revealed by 90 million impact craters
publisher	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/cb8a9e38289c4bd681296f17ff3947b5
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The Tharsis mantle source of depleted shergottites revealed by 90 million impact craters

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