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Innsbruckite, Mn33(Si2O5)14(OH)38 – a new mineral from the Tyrol, Austria

Published online by Cambridge University Press:  05 July 2018

Hannes Krüger ,
Peter Tropper ,
Udo Haefeker ,
Reinhard Kaindl ,
Martina Tribus ,
Volker Kahlenberg ,
Christoph Wikete ,
Martin R. Fuchs  and
Vincent Olieric
Hannes Krüger*
Affiliation:
Institute of Mineralogy and Petrography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria
Peter Tropper
Affiliation:
Institute of Mineralogy and Petrography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria
Udo Haefeker
Affiliation:
Institute of Mineralogy and Petrography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria
Reinhard Kaindl
Affiliation:
MATERIALS – Institute for Surface Technologies and Photonics, JOANNEUM RESEARCH Forschungsgesellschaft mbH, Leobner Strasse 94, 8712 Niklasdorf, Austria
Martina Tribus
Affiliation:
Institute of Mineralogy and Petrography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria
Volker Kahlenberg
Affiliation:
Institute of Mineralogy and Petrography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria
Christoph Wikete
Affiliation:
Material Technology Innsbruck (MTI), University of Innsbruck, Technikerstramße 13, 6020 Innsbruck, Austria
Martin R. Fuchs
Affiliation:
Swiss Light Source, Paul Scherrer Institute, 5232 Villigen, Switzerland
Vincent Olieric
Affiliation:
Swiss Light Source, Paul Scherrer Institute, 5232 Villigen, Switzerland
*
* E-mail: [email protected]
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Abstract

A description of the new mineral innsbruckite, Mn33(Si2O5)14(OH)38, a hydrous manganese phyllosilicate found in Tyrol, Austria is given. The crystal structure was determined by singlecrystal synchrotron radiation diffraction experiments at the X06DA beamline at the Swiss Light Source (Paul Scherrer Institute, Villigen, Switzerland). The space group is Cm and lattice parameters are a = 17.2760(19), b = 35.957(5), c = 7.2560(8) Å , β = 91.359(7)º, V = 4506.1(10) Å3, Z = 2. Innsbruckite belongs to the group of modulated 1:1 layer silicates and is chemically and structurally quite closely related to bementite, Mn7(Si2O5)3(OH)8. The chemical analysis revealed a close to ideal composition with only minor amounts of Al, Fe and Mg. Using Liebau’s nomenclature for silicate classification the silicate anion can be described as an unbranched siebener single layer. Innsbruckite shows a complex topology of the silicate sheet, exhibiting 4-, 5-, 6- and 8-membered rings. The silicate sheet is fully characterized using vertex symbols, and its topology is compared to those in other complex sheet silicates. Furthermore, the structural investigation is complemented with Raman spectroscopic studies.

Keywords

innsbruckitenew mineralphyllosilicateAustria
Type
Research Article
Information
Mineralogical Magazine , Volume 78 , Issue 7 , December 2014 , pp. 1613 - 1627
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2014

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Innsbruckite cif

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Innsbruckite cgd

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Innsbruckite arc

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