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Minerals of the arctite supergroup from the Bellerberg volcano xenoliths, Germany

Published online by Cambridge University Press:  26 August 2022

Rafał Juroszek Open the ORCID record for Rafał Juroszek [Opens in a new window] ,
Biljana Krüger Open the ORCID record for Biljana Krüger [Opens in a new window] ,
Beata Marciniak-Maliszewska Open the ORCID record for Beata Marciniak-Maliszewska [Opens in a new window]  and
Bernd Ternes
Rafał Juroszek*
Affiliation:
Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia, Będzińska 60, 41-205 Sosnowiec, Poland
Biljana Krüger
Affiliation:
Institute of Mineralogy and Petrography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria
Beata Marciniak-Maliszewska
Affiliation:
Faculty of Geology, University of Warsaw, Żwirki and Wigury 93, 02-089 Warsaw, Poland
Bernd Ternes
Affiliation:
Retired, Mayen, Germany
*
*Author for correspondence: Rafał Juroszek, Email: rafal.juroszek@us.edu.pl
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Abstract

The recently defined arctite supergroup contains nine mineral members defined as hexagonal intercalated antiperovskites, most of which have been found in pyrometamorphic rocks of the Hatrurim Complex, Israel. Three members of this supergroup: nabimusaite, gazeevite and zadovite, were identified for the first time in altered carbonate–silicate xenoliths from the Caspar and Scherer quarries, Bellerberg volcano in Germany. Present work focuses on the chemical, structural and spectroscopic investigation of these minerals and their correlation with holotype counterparts. The apparent differences are mainly related to the chemical composition, types of substitution in the tetrahedral and antiperovskite layers within the crystal structure, and position of bands in the Raman spectra. In the Bellerberg volcano xenoliths, the crystallisation of nabimusaite and gazeevite is caused by high-temperature alteration of early mineral associations (clinker-like phases) and their reaction with melt or gas generated by volcanic activity. In turn, the formation of zadovite is related to the Ba-rich silicate melt that filled the intergranular space between the rock-forming minerals.

Keywords

arctite supergroupnabimusaitegazeevitezadoviteBellerberg volcanoGermany
Type
Article
Information
Mineralogical Magazine , Volume 86 , Issue 6 , December 2022 , pp. 929 - 939
Copyright
Copyright © The Author(s), 2022. Published by Cambridge University Press on behalf of The Mineralogical Society of Great Britain and Ireland

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Footnotes

Associate Editor: Peter Leverett

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