Isotopic evolution of planetary crusts by hypervelocity impacts evidenced by Fe in microtektites

Fe isotopic composition of the distal ejecta of a terrestrial impact crater records both evaporation and condensation, refining the nature of the isotopic fractionation taking place during hypervelocity impacts in the Solar System.

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Autores principales:	S. M. Chernonozhkin, C. González de Vega, N. Artemieva, B. Soens, J. Belza, E. Bolea-Fernandez, M. Van Ginneken, B. P. Glass, L. Folco, M. J. Genge, Ph. Claeys, F. Vanhaecke, S. Goderis
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/651ef990918e42b592dd40ea2f625671
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spelling	oai:doaj.org-article:651ef990918e42b592dd40ea2f6256712021-12-02T15:15:14ZIsotopic evolution of planetary crusts by hypervelocity impacts evidenced by Fe in microtektites10.1038/s41467-021-25819-62041-1723https://doaj.org/article/651ef990918e42b592dd40ea2f6256712021-09-01T00:00:00Zhttps://doi.org/10.1038/s41467-021-25819-6https://doaj.org/toc/2041-1723Fe isotopic composition of the distal ejecta of a terrestrial impact crater records both evaporation and condensation, refining the nature of the isotopic fractionation taking place during hypervelocity impacts in the Solar System.S. M. ChernonozhkinC. González de VegaN. ArtemievaB. SoensJ. BelzaE. Bolea-FernandezM. Van GinnekenB. P. GlassL. FolcoM. J. GengePh. ClaeysF. VanhaeckeS. GoderisNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-12 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q S. M. Chernonozhkin C. González de Vega N. Artemieva B. Soens J. Belza E. Bolea-Fernandez M. Van Ginneken B. P. Glass L. Folco M. J. Genge Ph. Claeys F. Vanhaecke S. Goderis Isotopic evolution of planetary crusts by hypervelocity impacts evidenced by Fe in microtektites
description	Fe isotopic composition of the distal ejecta of a terrestrial impact crater records both evaporation and condensation, refining the nature of the isotopic fractionation taking place during hypervelocity impacts in the Solar System.
format	article
author	S. M. Chernonozhkin C. González de Vega N. Artemieva B. Soens J. Belza E. Bolea-Fernandez M. Van Ginneken B. P. Glass L. Folco M. J. Genge Ph. Claeys F. Vanhaecke S. Goderis
author_facet	S. M. Chernonozhkin C. González de Vega N. Artemieva B. Soens J. Belza E. Bolea-Fernandez M. Van Ginneken B. P. Glass L. Folco M. J. Genge Ph. Claeys F. Vanhaecke S. Goderis
author_sort	S. M. Chernonozhkin
title	Isotopic evolution of planetary crusts by hypervelocity impacts evidenced by Fe in microtektites
title_short	Isotopic evolution of planetary crusts by hypervelocity impacts evidenced by Fe in microtektites
title_full	Isotopic evolution of planetary crusts by hypervelocity impacts evidenced by Fe in microtektites
title_fullStr	Isotopic evolution of planetary crusts by hypervelocity impacts evidenced by Fe in microtektites
title_full_unstemmed	Isotopic evolution of planetary crusts by hypervelocity impacts evidenced by Fe in microtektites
title_sort	isotopic evolution of planetary crusts by hypervelocity impacts evidenced by fe in microtektites
publisher	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/651ef990918e42b592dd40ea2f625671
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Isotopic evolution of planetary crusts by hypervelocity impacts evidenced by Fe in microtektites

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