Experimental Etching of Diamonds: Extrapolation to Impact Diamonds from the Popigai Crater (Russia)

Diamond etching in high-temperature ambient-pressure experiments has been performed aimed to assess possible postimpact effects on diamonds in impact craters, for the case of the Popigai crater in Yakutia (Russia). The experiments with different etchants, including various combinations of silicate m...

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Autores principales: Valeri Sonin, Egor Zhimulev, Aleksei Chepurov, Ivan Gryaznov, Anatoly Chepurov, Valentin Afanasiev, Nikolai Pokhilenko
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Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/c4e393d1159047668b3c985175c17c6e
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spelling oai:doaj.org-article:c4e393d1159047668b3c985175c17c6e2021-11-25T18:26:27ZExperimental Etching of Diamonds: Extrapolation to Impact Diamonds from the Popigai Crater (Russia)10.3390/min111112292075-163Xhttps://doaj.org/article/c4e393d1159047668b3c985175c17c6e2021-11-01T00:00:00Zhttps://www.mdpi.com/2075-163X/11/11/1229https://doaj.org/toc/2075-163XDiamond etching in high-temperature ambient-pressure experiments has been performed aimed to assess possible postimpact effects on diamonds in impact craters, for the case of the Popigai crater in Yakutia (Russia). The experiments with different etchants, including various combinations of silicate melts, air, and inert gases, demonstrated the diversity of microstructures on {111} diamond faces: negative or positive trigons, as well as hexagonal, round, or irregularly shaped etch pits and striation. The surface features obtained after etching experiments with kimberlitic diamonds are similar to those observed on natural impact diamonds with some difference due to the origin of the latter as a result of a martensitic transformation of graphite in target rocks. Extrapolated to natural impact diamonds, the experimental results lead to several inferences: (1) Diamond crystals experienced natural oxidation and surface graphitization during the pressure decrease after the impact event, while the molten target rocks remained at high temperatures. (2) Natural etching of diamonds in silicate melts is possible in a large range of oxidation states controlled by O<sub>2</sub> diffusion. (3) Impact diamonds near the surface of molten target rocks oxidized at the highest rates, whereas those within the melt were shielded from the oxidizing agents and remained unchanged.Valeri SoninEgor ZhimulevAleksei ChepurovIvan GryaznovAnatoly ChepurovValentin AfanasievNikolai PokhilenkoMDPI AGarticleimpact diamondsetching experimentscrystal morphologyoxidationsurface graphitizationPopigai impact craterMineralogyQE351-399.2ENMinerals, Vol 11, Iss 1229, p 1229 (2021)
institution DOAJ
collection DOAJ
language EN
topic impact diamonds
etching experiments
crystal morphology
oxidation
surface graphitization
Popigai impact crater
Mineralogy
QE351-399.2
spellingShingle impact diamonds
etching experiments
crystal morphology
oxidation
surface graphitization
Popigai impact crater
Mineralogy
QE351-399.2
Valeri Sonin
Egor Zhimulev
Aleksei Chepurov
Ivan Gryaznov
Anatoly Chepurov
Valentin Afanasiev
Nikolai Pokhilenko
Experimental Etching of Diamonds: Extrapolation to Impact Diamonds from the Popigai Crater (Russia)
description Diamond etching in high-temperature ambient-pressure experiments has been performed aimed to assess possible postimpact effects on diamonds in impact craters, for the case of the Popigai crater in Yakutia (Russia). The experiments with different etchants, including various combinations of silicate melts, air, and inert gases, demonstrated the diversity of microstructures on {111} diamond faces: negative or positive trigons, as well as hexagonal, round, or irregularly shaped etch pits and striation. The surface features obtained after etching experiments with kimberlitic diamonds are similar to those observed on natural impact diamonds with some difference due to the origin of the latter as a result of a martensitic transformation of graphite in target rocks. Extrapolated to natural impact diamonds, the experimental results lead to several inferences: (1) Diamond crystals experienced natural oxidation and surface graphitization during the pressure decrease after the impact event, while the molten target rocks remained at high temperatures. (2) Natural etching of diamonds in silicate melts is possible in a large range of oxidation states controlled by O<sub>2</sub> diffusion. (3) Impact diamonds near the surface of molten target rocks oxidized at the highest rates, whereas those within the melt were shielded from the oxidizing agents and remained unchanged.
format article
author Valeri Sonin
Egor Zhimulev
Aleksei Chepurov
Ivan Gryaznov
Anatoly Chepurov
Valentin Afanasiev
Nikolai Pokhilenko
author_facet Valeri Sonin
Egor Zhimulev
Aleksei Chepurov
Ivan Gryaznov
Anatoly Chepurov
Valentin Afanasiev
Nikolai Pokhilenko
author_sort Valeri Sonin
title Experimental Etching of Diamonds: Extrapolation to Impact Diamonds from the Popigai Crater (Russia)
title_short Experimental Etching of Diamonds: Extrapolation to Impact Diamonds from the Popigai Crater (Russia)
title_full Experimental Etching of Diamonds: Extrapolation to Impact Diamonds from the Popigai Crater (Russia)
title_fullStr Experimental Etching of Diamonds: Extrapolation to Impact Diamonds from the Popigai Crater (Russia)
title_full_unstemmed Experimental Etching of Diamonds: Extrapolation to Impact Diamonds from the Popigai Crater (Russia)
title_sort experimental etching of diamonds: extrapolation to impact diamonds from the popigai crater (russia)
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/c4e393d1159047668b3c985175c17c6e
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