Low‐temperature dissociation of zircon in highly alkaline conditions: A cautionary note for studies on natural glasses of debated origin

Abstract Dissociated zircon is largely used as a robust indicator of glasses generated by impact cratering and airbursts. The reaction of zircon dissociation, i.e. ‘ZrSiO 4 → ZrO 2 + SiO 2 ’, requires high temperatures (>1670°C) only reached by extreme geological processes. Using high‐temperature experiments, this study shows that zircon can dissociate and form ZrO 2 ‐rich coronitic rims at temperatures of 900–1000°C (P = 1 bar), in the presence of a specific chemical environment made of NaCl or a mixture of NaCl and caliche soil (Ca‐sulfates). The use of silica glass vessels provides a SiO 2 ‐rich environment during the experiments. We observe that the dissociation is strongly related to the complexity of the surrounding system (e.g. the presence of other minerals that act as a flux) in which the reaction occurs. For these reasons, we suggest considering a more careful approach in using dissociated zircon as indicative of very high temperatures in glass‐forming processes.

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Publication Details

Journal
Meteoritics and Planetary Science
Published
2025-05-28
DOI
https://doi.org/10.1111/maps.14372
Primary Topic
Geological and Geochemical Analysis
Type
article
Field-Weighted Citation Impact
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article

Low‐temperature dissociation of zircon in highly alkaline conditions: A cautionary note for studies on natural glasses of debated origin

Anne‐Magali Seydoux‐Guillaume, Pierre-Marie Zanetta, Pierrick Roperch, Alexis Licht et al.
Meteoritics and Planetary Science
Geological and Geochemical Analysis
article

Low‐temperature dissociation of zircon in highly alkaline conditions: A cautionary note for studies on natural glasses of debated origin

Anne‐Magali Seydoux‐Guillaume, Pierre-Marie Zanetta, Pierrick Roperch, Alexis Licht, Daniel Ferry, P. Rochette, A. Musolino, Andréa Campos, Bertrand Devouard
article en

Abstract

Abstract Dissociated zircon is largely used as a robust indicator of glasses generated by impact cratering and airbursts. The reaction of zircon dissociation, i.e. ‘ZrSiO 4 → ZrO 2 + SiO 2 ’, requires high temperatures (>1670°C) only reached by extreme geological processes. Using high‐temperature experiments, this study shows that zircon can dissociate and form ZrO 2 ‐rich coronitic rims at temperatures of 900–1000°C (P = 1 bar), in the presence of a specific chemical environment made of NaCl or a mixture of NaCl and caliche soil (Ca‐sulfates). The use of silica glass vessels provides a SiO 2 ‐rich environment during the experiments. We observe that the dissociation is strongly related to the complexity of the surrounding system (e.g. the presence of other minerals that act as a flux) in which the reaction occurs. For these reasons, we suggest considering a more careful approach in using dissociated zircon as indicative of very high temperatures in glass‐forming processes.

Meteoritics and Planetary ScienceVol. 60(7)
Centre National de la Recherche Scientifique (FR), Aix-Marseille Université (FR), Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement (FR), Géosciences Rennes (FR), Centre de Recherche et d’Enseignement de Géosciences de l’Environnement (FR), Centrale Méditerranée (FR), Laboratoire de Géologie de Lyon : Terre, Planètes et Environnement (FR), Centre Interdisciplinaire de Nanoscience de Marseille (FR), Institut de Recherche pour le Développement (FR), Université de Rennes (FR), Université Jean Monnet (FR)
Agence Nationale de la Recherche
Life in Land
Openalex Percentile: Top 86%
Geological and Geochemical Analysis
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