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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Published in:Minerals
Main Authors: Valeri Sonin, Egor Zhimulev, Aleksei Chepurov, Ivan Gryaznov, Anatoly Chepurov, Valentin Afanasiev, Nikolai Pokhilenko
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/min11111229
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spelling ftmdpi:oai:mdpi.com:/2075-163X/11/11/1229/ 2023-08-20T04:10:20+02:00 Experimental Etching of Diamonds: Extrapolation to Impact Diamonds from the Popigai Crater (Russia) Valeri Sonin Egor Zhimulev Aleksei Chepurov Ivan Gryaznov Anatoly Chepurov Valentin Afanasiev Nikolai Pokhilenko agris 2021-11-05 application/pdf https://doi.org/10.3390/min11111229 EN eng Multidisciplinary Digital Publishing Institute Mineral Deposits https://dx.doi.org/10.3390/min11111229 https://creativecommons.org/licenses/by/4.0/ Minerals; Volume 11; Issue 11; Pages: 1229 impact diamonds etching experiments crystal morphology oxidation surface graphitization Popigai impact crater Text 2021 ftmdpi https://doi.org/10.3390/min11111229 2023-08-01T03:10:19Z 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 O2 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. Text Yakutia MDPI Open Access Publishing Minerals 11 11 1229
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic impact diamonds
etching experiments
crystal morphology
oxidation
surface graphitization
Popigai impact crater
spellingShingle impact diamonds
etching experiments
crystal morphology
oxidation
surface graphitization
Popigai impact crater
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)
topic_facet impact diamonds
etching experiments
crystal morphology
oxidation
surface graphitization
Popigai impact crater
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 O2 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 Text
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 Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/min11111229
op_coverage agris
genre Yakutia
genre_facet Yakutia
op_source Minerals; Volume 11; Issue 11; Pages: 1229
op_relation Mineral Deposits
https://dx.doi.org/10.3390/min11111229
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/min11111229
container_title Minerals
container_volume 11
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container_start_page 1229
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