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FRIGN zircon—The only terrestrial mineral diagnostic of high-pressure and high-temperature shock deformation

Authors :
Nicholas E. Timms
Ludovic Ferrière
Aaron J. Cavosie
Pierre Rochette
Curtin University [Perth]
Planning and Transport Research Centre (PATREC)
The Natural History Museum [London] (NHM)
Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE)
Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Collège de France (CdF (institution))-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS)-Institut National de la Recherche Agronomique (INRA)
NASA Astrobiology program [NNAI3AA94A]
Microscopy and Microanalysis Facility at Curtin University, Australia
Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Source :
Geology, Geology, Geological Society of America, 2018, 46 (10), pp.891-894. ⟨10.1130/G45079.1⟩, Geology, 2018, 46 (10), pp.891-894. ⟨10.1130/G45079.1⟩
Publication Year :
2018
Publisher :
Geological Society of America, 2018.

Abstract

International audience; Minerals that record high-pressure deformation from meteorite impact are relatively common on Earth; however, minerals that record both high-pressure and high-temperature effects of impact are rare, and they occur mostly in meteorites. Here, we report new occurrences of a type of granular zircon that is the only terrestrial mineral known that uniquely records both high-pressure and high-temperature conditions diagnostic of impact. Granular zircon grains in impact melt rock from the Luizi impact structure (Democratic Republic of the Congo) and in glass from the recently described Pantasma structure (Nicaragua) consist of similar to 1-mu m-sized neoblasts in multiple domains that are systematically oriented such that all (001) poles are approximately orthogonal and coincide with a direction from adjacent domains. The neoblast orientations are produced uniquely by transformation to the high-pressure polymorph reidite and its subsequent reversion to neoblastic zircon at high-temperature conditions, as evidenced by the occurrence of ZrO2. We here refer to such granular grains that preserve orientation evidence for reversion from reidite as "former reidite in granular neoblastic" zircon, or FRIGN zircon, in order to distinguish this type of granular zircon from those that do not record high-pressure conditions. In addition to the localities described here, examples of what can now be classified as FRIGN zircon have been documented at Meteor Crater (Barringer crater, USA), at the Acraman impact structure (Australia), and in Australasian tektites. Occurrences thus span five continents, range in age from Precambrian (ca. 590 Ma) to recent (ca. 49 ka), and serve as a diagnostic indicator of impact metamorphism that may be present throughout much of the geological record. FRIGN zircon further has potential to be found in extraterrestrial samples, where granular zircon has previously been reported.

Details

ISSN :
00917613
Volume :
46
Database :
OpenAIRE
Journal :
Geology
Accession number :
edsair.doi.dedup.....a0086b5548b795e55c00992811c18304
Full Text :
https://doi.org/10.1130/g45079.1