A large planetary body inferred from diamond inclusions in a ureilite meteorite

Ureilites are a type of meteorite that are believed to be derived from a parent body that was impacted in the early solar system. Here, the authors analyse inclusions within diamonds from a ureilite meteorite and find that they must have formed at above 20 GPa suggesting the parent body was Mercury-...

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Autores principales:	Farhang Nabiei, James Badro, Teresa Dennenwaldt, Emad Oveisi, Marco Cantoni, Cécile Hébert, Ahmed El Goresy, Jean-Alix Barrat, Philippe Gillet
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/b4c2bde440254a8e830f0faa39f1eca6
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spelling	oai:doaj.org-article:b4c2bde440254a8e830f0faa39f1eca62021-12-02T15:33:57ZA large planetary body inferred from diamond inclusions in a ureilite meteorite10.1038/s41467-018-03808-62041-1723https://doaj.org/article/b4c2bde440254a8e830f0faa39f1eca62018-04-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-03808-6https://doaj.org/toc/2041-1723Ureilites are a type of meteorite that are believed to be derived from a parent body that was impacted in the early solar system. Here, the authors analyse inclusions within diamonds from a ureilite meteorite and find that they must have formed at above 20 GPa suggesting the parent body was Mercury- to Mars-sized.Farhang NabieiJames BadroTeresa DennenwaldtEmad OveisiMarco CantoniCécile HébertAhmed El GoresyJean-Alix BarratPhilippe GilletNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-6 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Farhang Nabiei James Badro Teresa Dennenwaldt Emad Oveisi Marco Cantoni Cécile Hébert Ahmed El Goresy Jean-Alix Barrat Philippe Gillet A large planetary body inferred from diamond inclusions in a ureilite meteorite
description	Ureilites are a type of meteorite that are believed to be derived from a parent body that was impacted in the early solar system. Here, the authors analyse inclusions within diamonds from a ureilite meteorite and find that they must have formed at above 20 GPa suggesting the parent body was Mercury- to Mars-sized.
format	article
author	Farhang Nabiei James Badro Teresa Dennenwaldt Emad Oveisi Marco Cantoni Cécile Hébert Ahmed El Goresy Jean-Alix Barrat Philippe Gillet
author_facet	Farhang Nabiei James Badro Teresa Dennenwaldt Emad Oveisi Marco Cantoni Cécile Hébert Ahmed El Goresy Jean-Alix Barrat Philippe Gillet
author_sort	Farhang Nabiei
title	A large planetary body inferred from diamond inclusions in a ureilite meteorite
title_short	A large planetary body inferred from diamond inclusions in a ureilite meteorite
title_full	A large planetary body inferred from diamond inclusions in a ureilite meteorite
title_fullStr	A large planetary body inferred from diamond inclusions in a ureilite meteorite
title_full_unstemmed	A large planetary body inferred from diamond inclusions in a ureilite meteorite
title_sort	large planetary body inferred from diamond inclusions in a ureilite meteorite
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/b4c2bde440254a8e830f0faa39f1eca6
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A large planetary body inferred from diamond inclusions in a ureilite meteorite

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