Rüdlingerite, Mn<sup>2+</sup><sub>2</sub>V<sup>5+</sup>As<sup>5+</sup>O<sub>7</sub>·2H<sub>2</sub>O, a New Species Isostructural with Fianelite
The new mineral species rüdlingerite, ideally Mn<sup>2+</sup><sub>2</sub>V<sup>5+</sup>As<sup>5+</sup>O<sub>7</sub>·2H<sub>2</sub>O, occurs in the Fianel mine, in Val Ferrera, Grisons, Switzerland, a small Alpine metamorphic Mn...
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MDPI AG
2020-10-01
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DOAJ |
language |
English |
format |
Article |
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DOAJ |
author |
Philippe Roth Nicolas Meisser Fabrizio Nestola Radek Škoda Fernando Cámara Ferdinando Bosi Marco E. Ciriotti Ulf Hålenius Cédric Schnyder Roberto Bracco |
spellingShingle |
Philippe Roth Nicolas Meisser Fabrizio Nestola Radek Škoda Fernando Cámara Ferdinando Bosi Marco E. Ciriotti Ulf Hålenius Cédric Schnyder Roberto Bracco Rüdlingerite, Mn<sup>2+</sup><sub>2</sub>V<sup>5+</sup>As<sup>5+</sup>O<sub>7</sub>·2H<sub>2</sub>O, a New Species Isostructural with Fianelite Minerals rüdlingerite new mineral species fianelite vanadium arsenic crystal structure |
author_facet |
Philippe Roth Nicolas Meisser Fabrizio Nestola Radek Škoda Fernando Cámara Ferdinando Bosi Marco E. Ciriotti Ulf Hålenius Cédric Schnyder Roberto Bracco |
author_sort |
Philippe Roth |
title |
Rüdlingerite, Mn<sup>2+</sup><sub>2</sub>V<sup>5+</sup>As<sup>5+</sup>O<sub>7</sub>·2H<sub>2</sub>O, a New Species Isostructural with Fianelite |
title_short |
Rüdlingerite, Mn<sup>2+</sup><sub>2</sub>V<sup>5+</sup>As<sup>5+</sup>O<sub>7</sub>·2H<sub>2</sub>O, a New Species Isostructural with Fianelite |
title_full |
Rüdlingerite, Mn<sup>2+</sup><sub>2</sub>V<sup>5+</sup>As<sup>5+</sup>O<sub>7</sub>·2H<sub>2</sub>O, a New Species Isostructural with Fianelite |
title_fullStr |
Rüdlingerite, Mn<sup>2+</sup><sub>2</sub>V<sup>5+</sup>As<sup>5+</sup>O<sub>7</sub>·2H<sub>2</sub>O, a New Species Isostructural with Fianelite |
title_full_unstemmed |
Rüdlingerite, Mn<sup>2+</sup><sub>2</sub>V<sup>5+</sup>As<sup>5+</sup>O<sub>7</sub>·2H<sub>2</sub>O, a New Species Isostructural with Fianelite |
title_sort |
rüdlingerite, mn<sup>2+</sup><sub>2</sub>v<sup>5+</sup>as<sup>5+</sup>o<sub>7</sub>·2h<sub>2</sub>o, a new species isostructural with fianelite |
publisher |
MDPI AG |
series |
Minerals |
issn |
2075-163X |
publishDate |
2020-10-01 |
description |
The new mineral species rüdlingerite, ideally Mn<sup>2+</sup><sub>2</sub>V<sup>5+</sup>As<sup>5+</sup>O<sub>7</sub>·2H<sub>2</sub>O, occurs in the Fianel mine, in Val Ferrera, Grisons, Switzerland, a small Alpine metamorphic Mn deposit. It is associated with ansermetite and Fe oxyhydroxide in thin fractures in Triassic dolomitic marbles. Rüdlingerite was also found in specimens recovered from the dump of the Valletta mine, Canosio, Cuneo, Piedmont, Italy, where it occurs together with massive braccoite and several other As- and V-rich phases in richly mineralized veins crossing the quartz-hematite ore. The new mineral displays at both localities yellow to orange, flattened elongated prismatic, euhedral crystals measuring up to 300 μm in length. Electron-microprobe analysis of rüdlingerite from Fianel gave (in wt%): MnO 36.84, FeO 0.06, As<sub>2</sub>O<sub>5</sub>, 25.32, V<sub>2</sub>O<sub>5</sub> 28.05, SiO<sub>2</sub> 0.13, H<sub>2</sub>O<sub>calc</sub> 9.51, total 99.91. On the basis of 9 O anions per formula unit, the chemical formula of rüdlingerite is Mn<sub>1.97</sub>(V<sup>5+</sup><sub>1.17</sub> As<sub>0.83</sub>Si<sub>0.01</sub>)<sub>Σ2.01</sub>O<sub>7</sub>·2H<sub>2</sub>O. The main diffraction lines are [<i>d<sub>obs</sub></i> in Å (<i>I<sub>obs</sub></i>) <i>hkl</i>]: 3.048 (100) 022, 5.34 (80) 120, 2.730 (60) 231, 2.206 (60) 16-1, 7.28 (50) 020, 2.344 (50) 250, 6.88 (40) 110, and 2.452 (40) 320. Study of the crystal structure showcases a monoclinic unit cell, space group <i>P</i>2<sub>1</sub><i>/n</i>, with <i>a</i> = 7.8289(2) Å, <i>b</i> = 14.5673(4) Å, <i>c</i> = 6.7011(2) Å, <i>β</i> = 93.773(2)°, <i>V</i> = 762.58(4) Å<sup>3</sup>, <i>Z</i> = 4. The crystal structure has been solved and refined to <i>R</i><sub>1</sub> = 0.041 on the basis of 3784 reflections with <i>F</i><sub>o</sub> > 4σ(<i>F</i>). It shows Mn<sup>2+</sup> hosted in chains of octahedra that are subparallel to [-101] and bound together by pairs of tetrahedra hosted by V<sup>5+</sup> and As<sup>5+</sup>, building up a framework. Additional linkage is provided by hydrogen-bonding through H<sub>2</sub>O coordinating Mn<sup>2+</sup> at the octahedra. One tetrahedrally coordinated site is dominated by V<sup>5+</sup>, <i><sup>T</sup></i><sup>(1)</sup>(V<sub>0.88</sub>As<sub>0.12</sub>), corresponding to an observed site scattering of 24.20 electrons per site (eps), whereas the second site is strongly dominated by As<sup>5+</sup>,<i><sup> T</sup></i><sup>(2)</sup>(As<sub>0.74</sub>V<sub>0.26</sub>), with, accordingly, a higher observed site scattering of 30.40 eps. The new mineral has been approved by the IMA-CNMNC and named for Gottfried Rüdlinger (born 1919), a pioneer in the 1960–1980s, in the search and study of the small minerals from the Alpine manganese mineral deposits of Grisons. |
topic |
rüdlingerite new mineral species fianelite vanadium arsenic crystal structure |
url |
https://www.mdpi.com/2075-163X/10/11/960 |
work_keys_str_mv |
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doaj-bbe75bcc5b1f4bc2aedce3ac23d286b52020-11-25T04:06:12ZengMDPI AGMinerals2075-163X2020-10-011096096010.3390/min10110960Rüdlingerite, Mn<sup>2+</sup><sub>2</sub>V<sup>5+</sup>As<sup>5+</sup>O<sub>7</sub>·2H<sub>2</sub>O, a New Species Isostructural with FianelitePhilippe Roth0Nicolas Meisser1Fabrizio Nestola2Radek Škoda3Fernando Cámara4Ferdinando Bosi5Marco E. Ciriotti6Ulf Hålenius7Cédric Schnyder8Roberto Bracco9Swiss Seismological Service, ETH Zürich, 8092 Zurich, SwitzerlandMusée cantonal de géologie, Université de Lausanne, 1015 Lausanne, SwitzerlandDipartimento di Geoscienze, Università degli studi di Padova, 35131 Padova, ItalyDepartment of Geological Sciences, Masaryk University, 611 37 Brno, Czech RepublicDipartimento di Scienze della Terra, Università degli Studi di Milano, 20133 Milano, ItalyDipartimento di Scienze della Terra, Sapienza Università di Roma, 00185 Rome, ItalyDipartimento di Scienze della Terra, Università degli Studi di Torino, 10125 Torino, ItalyDepartment of Geosciences, Swedish Museum of Natural History, 10405 Stockholm, SwedenMusée cantonal de géologie, Université de Lausanne, 1015 Lausanne, SwitzerlandAssociazione Micromineralogica Italiana, 17100 Savona, ItalyThe new mineral species rüdlingerite, ideally Mn<sup>2+</sup><sub>2</sub>V<sup>5+</sup>As<sup>5+</sup>O<sub>7</sub>·2H<sub>2</sub>O, occurs in the Fianel mine, in Val Ferrera, Grisons, Switzerland, a small Alpine metamorphic Mn deposit. It is associated with ansermetite and Fe oxyhydroxide in thin fractures in Triassic dolomitic marbles. Rüdlingerite was also found in specimens recovered from the dump of the Valletta mine, Canosio, Cuneo, Piedmont, Italy, where it occurs together with massive braccoite and several other As- and V-rich phases in richly mineralized veins crossing the quartz-hematite ore. The new mineral displays at both localities yellow to orange, flattened elongated prismatic, euhedral crystals measuring up to 300 μm in length. Electron-microprobe analysis of rüdlingerite from Fianel gave (in wt%): MnO 36.84, FeO 0.06, As<sub>2</sub>O<sub>5</sub>, 25.32, V<sub>2</sub>O<sub>5</sub> 28.05, SiO<sub>2</sub> 0.13, H<sub>2</sub>O<sub>calc</sub> 9.51, total 99.91. On the basis of 9 O anions per formula unit, the chemical formula of rüdlingerite is Mn<sub>1.97</sub>(V<sup>5+</sup><sub>1.17</sub> As<sub>0.83</sub>Si<sub>0.01</sub>)<sub>Σ2.01</sub>O<sub>7</sub>·2H<sub>2</sub>O. The main diffraction lines are [<i>d<sub>obs</sub></i> in Å (<i>I<sub>obs</sub></i>) <i>hkl</i>]: 3.048 (100) 022, 5.34 (80) 120, 2.730 (60) 231, 2.206 (60) 16-1, 7.28 (50) 020, 2.344 (50) 250, 6.88 (40) 110, and 2.452 (40) 320. Study of the crystal structure showcases a monoclinic unit cell, space group <i>P</i>2<sub>1</sub><i>/n</i>, with <i>a</i> = 7.8289(2) Å, <i>b</i> = 14.5673(4) Å, <i>c</i> = 6.7011(2) Å, <i>β</i> = 93.773(2)°, <i>V</i> = 762.58(4) Å<sup>3</sup>, <i>Z</i> = 4. The crystal structure has been solved and refined to <i>R</i><sub>1</sub> = 0.041 on the basis of 3784 reflections with <i>F</i><sub>o</sub> > 4σ(<i>F</i>). It shows Mn<sup>2+</sup> hosted in chains of octahedra that are subparallel to [-101] and bound together by pairs of tetrahedra hosted by V<sup>5+</sup> and As<sup>5+</sup>, building up a framework. Additional linkage is provided by hydrogen-bonding through H<sub>2</sub>O coordinating Mn<sup>2+</sup> at the octahedra. One tetrahedrally coordinated site is dominated by V<sup>5+</sup>, <i><sup>T</sup></i><sup>(1)</sup>(V<sub>0.88</sub>As<sub>0.12</sub>), corresponding to an observed site scattering of 24.20 electrons per site (eps), whereas the second site is strongly dominated by As<sup>5+</sup>,<i><sup> T</sup></i><sup>(2)</sup>(As<sub>0.74</sub>V<sub>0.26</sub>), with, accordingly, a higher observed site scattering of 30.40 eps. The new mineral has been approved by the IMA-CNMNC and named for Gottfried Rüdlinger (born 1919), a pioneer in the 1960–1980s, in the search and study of the small minerals from the Alpine manganese mineral deposits of Grisons.https://www.mdpi.com/2075-163X/10/11/960rüdlingeritenew mineral speciesfianelitevanadiumarseniccrystal structure |