Nickel isotopic evidence for late-stage accretion of Mercury-like differentiated planetary embryos

Based on Nickel isotope analysis of meteorites and terrestrial rocks, the authors suggest that the Bulk Silicate Earth has a sub-chondritic Nickel isotope composition. This signature is thought to result from the impact and accretion of a Mercury-like impactor which originated from the innermost Sol...

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Autores principales:	Shui-Jiong Wang, Wenzhong Wang, Jian-Ming Zhu, Zhongqing Wu, Jingao Liu, Guilin Han, Fang-Zhen Teng, Shichun Huang, Hongjie Wu, Yujian Wang, Guangliang Wu, Weihan Li
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/9755a107c94743429ce17f551e04c3c7
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spelling	oai:doaj.org-article:9755a107c94743429ce17f551e04c3c72021-12-02T14:01:14ZNickel isotopic evidence for late-stage accretion of Mercury-like differentiated planetary embryos10.1038/s41467-020-20525-12041-1723https://doaj.org/article/9755a107c94743429ce17f551e04c3c72021-01-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-20525-1https://doaj.org/toc/2041-1723Based on Nickel isotope analysis of meteorites and terrestrial rocks, the authors suggest that the Bulk Silicate Earth has a sub-chondritic Nickel isotope composition. This signature is thought to result from the impact and accretion of a Mercury-like impactor which originated from the innermost Solar System.Shui-Jiong WangWenzhong WangJian-Ming ZhuZhongqing WuJingao LiuGuilin HanFang-Zhen TengShichun HuangHongjie WuYujian WangGuangliang WuWeihan LiNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-7 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Shui-Jiong Wang Wenzhong Wang Jian-Ming Zhu Zhongqing Wu Jingao Liu Guilin Han Fang-Zhen Teng Shichun Huang Hongjie Wu Yujian Wang Guangliang Wu Weihan Li Nickel isotopic evidence for late-stage accretion of Mercury-like differentiated planetary embryos
description	Based on Nickel isotope analysis of meteorites and terrestrial rocks, the authors suggest that the Bulk Silicate Earth has a sub-chondritic Nickel isotope composition. This signature is thought to result from the impact and accretion of a Mercury-like impactor which originated from the innermost Solar System.
format	article
author	Shui-Jiong Wang Wenzhong Wang Jian-Ming Zhu Zhongqing Wu Jingao Liu Guilin Han Fang-Zhen Teng Shichun Huang Hongjie Wu Yujian Wang Guangliang Wu Weihan Li
author_facet	Shui-Jiong Wang Wenzhong Wang Jian-Ming Zhu Zhongqing Wu Jingao Liu Guilin Han Fang-Zhen Teng Shichun Huang Hongjie Wu Yujian Wang Guangliang Wu Weihan Li
author_sort	Shui-Jiong Wang
title	Nickel isotopic evidence for late-stage accretion of Mercury-like differentiated planetary embryos
title_short	Nickel isotopic evidence for late-stage accretion of Mercury-like differentiated planetary embryos
title_full	Nickel isotopic evidence for late-stage accretion of Mercury-like differentiated planetary embryos
title_fullStr	Nickel isotopic evidence for late-stage accretion of Mercury-like differentiated planetary embryos
title_full_unstemmed	Nickel isotopic evidence for late-stage accretion of Mercury-like differentiated planetary embryos
title_sort	nickel isotopic evidence for late-stage accretion of mercury-like differentiated planetary embryos
publisher	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/9755a107c94743429ce17f551e04c3c7
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Nickel isotopic evidence for late-stage accretion of Mercury-like differentiated planetary embryos

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