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tuperssuatsiaite

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Journal Article

The structure of Mn-rich tuperssuatsiaite: A palygorskite-related mineral

Fernando Cámara, Laurence A.J. Garvie, Bertrand Devouard, Thomas L. Groy, Peter R. Buseck
Published: 01 October 2002
American Mineralogist (2002) 87 (10): 1458–1463.
DOI: https://doi.org/10.2138/am-2002-1023
...Fernando Cámara; Laurence A.J. Garvie; Bertrand Devouard; Thomas L. Groy; Peter R. Buseck Abstract The structure of tuperssuatsiaite from the Aris phonolite in central Namibia was refined to an R index of 0.075 for 905 observed reflections [ I > 2σ( I )] obtained with a four-circle X-ray...
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Lattice parameter ( a ) a and ( b ) β vs. the average ionic radii (< r...

Lattice parameter ( a ) a and ( b ) β vs. the average ionic radii (< r...

Published: 01 October 2002
F igure 4. Lattice parameter ( a ) a and ( b ) β vs. the average ionic radii (< r >) in the M1 + M2 sites for tuperssuatsiaite compared with data for raite, palygorskite, and tuperssuatsiaite. Symbols as follows: full dot = palygorskite, Grobéty et al. (1995) ; full triangle = raite
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Arrangement of octahedral sites in the crystal structures of windhoekite (l...

Arrangement of octahedral sites in the crystal structures of windhoekite (l...

Published: 01 January 2012
Fig. 6 Arrangement of octahedral sites in the crystal structures of windhoekite (left) and tuperssuatsiaite (right) projected on (100). An additional Ca2 ( M 4) site is present in the structure of windhoekite but missing in the structure of tuperssuatsiaite. Note that all outer corners of Ca1
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Polyhedral representation of the crystal structures of windhoekite (left) a...

Polyhedral representation of the crystal structures of windhoekite (left) a...

Published: 01 January 2012
Fig. 5 Polyhedral representation of the crystal structures of windhoekite (left) and tuperssuatsiaite (right) projected on (001). Light grey octahedra correspond to Fe sites M 1 and M 2; dark grey octahedra correspond to Ca-dominant sites M 3 and M 4 in windhoekite and Na-dominant site
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Ellingsenite (1), <span class="search-highlight">tuperssuatsiaite</span> (2), villiaumite (3), tobermorite (4), n...

Ellingsenite (1), tuperssuatsiaite (2), villiaumite (3), tobermorite (4), n...

Published: 01 October 2011
Fig. 2 Ellingsenite (1), tuperssuatsiaite (2), villiaumite (3), tobermorite (4), natrolite (5) and aegirine (6) in a vesicle within phonolite.
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<span class="search-highlight">Tuperssuatsiaite</span> sprays in a vug. The smaller dark laths are aegerine and t...

Tuperssuatsiaite sprays in a vug. The smaller dark laths are aegerine and t...

Published: 01 October 2002
F igure 1. Tuperssuatsiaite sprays in a vug. The smaller dark laths are aegerine and the clear crystals are zeolites. The scale bar is 1 mm in length.
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[100] zone axis SAED pattern of <span class="search-highlight">tuperssuatsiaite</span>.

[100] zone axis SAED pattern of tuperssuatsiaite.

Published: 01 October 2002
F igure 2. [100] zone axis SAED pattern of tuperssuatsiaite.
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The structure of <span class="search-highlight">tuperssuatsiaite</span> projected ( a ) along [100] and ( b ) alo...

The structure of tuperssuatsiaite projected ( a ) along [100] and ( b ) alo...

Published: 01 October 2002
F igure 3. The structure of tuperssuatsiaite projected ( a ) along [100] and ( b ) along [001].
Journal Article

Windhoekite, Ca 2 Fe 3+ 3− x (Si 8 O 20 )(OH) 4 ·10H 2 O, a new palygorskite-group mineral from the Aris phonolite, Namibia

Nikita V. Chukanov, Sergey N. Britvin, Günter Blass, Dmitriy I. Belakovskiy, Konstantin V. Van
Published: 01 January 2012
European Journal of Mineralogy (2012) 24 (1): 171–179.
DOI: https://doi.org/10.1127/0935-1221/2011/0023-2161
...Fig. 6 Arrangement of octahedral sites in the crystal structures of windhoekite (left) and tuperssuatsiaite (right) projected on (100). An additional Ca2 ( M 4) site is present in the structure of windhoekite but missing in the structure of tuperssuatsiaite. Note that all outer corners of Ca1...
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Infrared spectra of palygorskite-group minerals: windhoekite (a), tuperssua...

Infrared spectra of palygorskite-group minerals: windhoekite (a), tuperssua...

Published: 01 January 2012
Fig. 4 Infrared spectra of palygorskite-group minerals: windhoekite (a), tuperssuatsiaite from Aris, Namibia (b), palygorskite from Penchi, China (c), and yofortierite from Mt. Karnasurt, Lovozero massif, Kola peninsula, Russia (d).
Journal Article

Windmountainite, □Fe 3+ 2 Mg 2 □ 2 Si 8 O 20 (OH) 2 (H 2 O) 4 ·4H 2 O, a new modulated, layered Fe 3+ -Mg-silicate-hydrate from Wind Mountain, New Mexico: Characterization and origin, with comments on the classification of palygorskite-group minerals

Derek D. Leung, Andrew M. McDonald
Published: 01 July 2020
The Canadian Mineralogist (2020) 58 (4): 477–509.
DOI: https://doi.org/10.3749/canmin.1900063
...) 2 (H 2 O,OH) 4 · W ] is proposed based on the occupants of the four M sites. Within this scheme, windmountainite is the □-Fe 3+ -Mg-□ member. The palygorskite group includes six members: palygorskite (monoclinic and orthorhombic polytypes), yofortierite, tuperssuatsiaite, raite, windhoekite...
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Sazhinite-(La), Na 3 LaSi 6 O 15 (H 2 O) 2 , a new mineral from the Aris phonolite, Namibia: Description and crystal structure

F. Cámara, L. Ottolini, B. Devouard, L. A. J. Garvie, F. C. Hawthorne
Published: 01 August 2006
Mineralogical Magazine (2006) 70 (4): 405–418.
DOI: https://doi.org/10.1180/0026461067040343
..., microcline, apophyllite, sphalerite, analcime, fluorite, villiaumite, hydroxylapatite, galena, makatite, quartz, eudialyte, kanemite, tuperssuatsiaite and korobitsynite. Sazhinite-(La) forms small euhedral crystals up to 1 mm long and 0.4 mm wide, elongated along [001] and flattened on (010), exhibiting...
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JOHNSENITE-(Ce): A NEW MEMBER OF THE EUDIALYTE GROUP FROM MONT SAINT-HILAIRE, QUEBEC, CANADA

Joel D. Grice, Robert A. Gault
Published: 01 February 2006
The Canadian Mineralogist (2006) 44 (1): 105–115.
DOI: https://doi.org/10.2113/gscanmin.44.1.105
..., stillwellite-(Ce), titanite, cerite-(Ce), tuperssuatsiaite, steacyite, catapleiite, zakharovite, natrolite and microcline. It is transparent to translucent with a vitreous luster and white streak. It is brittle with a Mohs hardness of 5–6. It has no discernable cleavage or parting and an uneven fracture...
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THE CRYSTAL STRUCTURE OF YOFORTIERITE

Frank C. Hawthorne, Yassir A. Abdu, Kimberly T. Tait, Malcolm E. Back
Published: 01 April 2013
The Canadian Mineralogist (2013) 51 (2): 243–251.
DOI: https://doi.org/10.3749/canmin.51.2.243
... absorption corrections (SADABS; Sheldrick 2008 ) were applied and identical data merged to give 7519 reflections covering the entire Ewald sphere and 1946 unique reflections with R merge = 1.5%. As with tuperssuatsiaite ( Cámara et al . 2002 ), there are numerous weak reflections violating the C...
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Niobium Is Highly Mobile As a Polyoxometalate Ion During Natural Weathering

Henrik Friis, William H. Casey
Published: 01 November 2018
The Canadian Mineralogist (2018) 56 (6): 905–912.
DOI: https://doi.org/10.3749/canmin.1800058
.... Lueshite appears to be one of the last-formed minerals and can be very abundant, covering most of some natrolite cavities. The same natrolite paragenesis also hosts tuperssuatsiaite and aegirine. A pyrochlore group mineral and fersmite on hydroxylgugiaite from an altered pegmatite on Mount Nakkaalaaq...
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Rock-Forming Minerals, Vol. 3c, Sheet Silicates–Clay Minerals , 2 nd edition

George E. Christidis
Journal: Clay Minerals
Published: 01 December 2014
Clay Minerals (2014) 49 (5): 765–766.
.... On the other hand, certain clay minerals have not been considered, including imogolite (but not allophane), volkonskoite and minerals of the sepiolite-palygorskite group with the exception of loughlinite (falcondoite, kalifersite, raite, tuperssuatsiaite, and yofortierite). Although, with the exception...
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BOOK REVIEW

Stephen Guggenheim
Published: 01 December 2013
Clays and Clay Minerals (2013) 61 (5): 475–476.
.... yofortierite, windhoekite, tuperssuatsiaite, raite, several of which have single-crystal, X-ray determinations of their structures). Although loughlinite (Na-rich sepiolite) is mentioned under sepiolite, no mention is made of these other minerals, not even in the chemistry description for palygorskite...
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Synchrotron powder X-ray diffraction study of the structure and dehydration behavior of palygorskite

Jeffrey E. Post, Peter J. Heaney
Published: 01 April 2008
American Mineralogist (2008) 93 (4): 667–675.
DOI: https://doi.org/10.2138/am.2008.2590
... positions, displacement factors, and occupancy factors of the O atoms of the H 2 O molecules were refined. Soft constraints were used to limit the Si-O bond distances to within the range observed in similar silicate structures, e.g., tuperssuatsiaite (1.58–1.63 Å, <1.61 Å>; Cámara et al. 2002...
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ARISITE-(Ce), A NEW RARE-EARTH FLUORCARBONATE FROM THE ARIS PHONOLITE, NAMIBIA, MONT SAINT-HILAIRE AND THE SAINT-AMABLE SILL, QUEBEC, CANADA

Paula C. Piilonen, Andrew M. McDonald, Joel D. Grice, Ralph Rowe, Robert A. Gault, Glenn Poirier, Mark A. Cooper, Uwe Kolitsch, Andrew C. Roberts, William Lechner, Andreas G. Palfi
Published: 01 June 2010
The Canadian Mineralogist (2010) 48 (3): 661–671.
DOI: https://doi.org/10.3749/canmin.48.3.661
... that 15–20% of the phonolite is comprised of two-phase fluid + vapor-filled cavities. The miarolitic cavities host a range of agpaitic mineral species, including abundant villiaumite, aegirine, labuntsovite-group minerals, tuperssuatsiaite, natrolite, analcime, manganoneptunite, apophyllite-(KF), fluorite...
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ELLINGSENITE, Na 5 Ca 6 Si 18 O 38 (OH) 13 ·6H 2 O, A NEW MARTINITE-RELATED MINERAL SPECIES FROM PHONOLITE OF THE ARIS ALKALINE COMPLEX, NAMIBIA

Victor N. Yakovenchuk, Gregory Yu. Ivanyuk, Yakov A. Pakhomovsky, Ekaterina A. Selivanova, Julia A. Mikhailova, Sergey V. Krivovichev, Andrey A. Zolotarev, Oleg A. Zalkind
Published: 01 October 2011
The Canadian Mineralogist (2011) 49 (5): 1165–1173.
DOI: https://doi.org/10.3749/canmin.49.5.1165
...Fig. 2 Ellingsenite (1), tuperssuatsiaite (2), villiaumite (3), tobermorite (4), natrolite (5) and aegirine (6) in a vesicle within phonolite. ...
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