Cyprine, ideally Ca19Cu2+(Al,Mg,Mn)12Si18O69(OH)9, was found at the Wessels mine near Hotazel, Kalahari Manganese Field, North Cape province, South Africa. It occurs as chaotic aggregates (up to 5 cm across) in open cavities or embedded in coarse-grained colourless calcite. Associated minerals are calcite, apatite, andradite, henritermierite and rhodochrosite. Single crystals of cyprine up to 1 cm are dark red with a lilac hue and vitreous lustre. Dominant crystal forms are {1 0 0}, {1 1 0} and {3 3 1}. The Mohs hardness is 6.5. Dmeas and Dcalc are 3.40(3) and 3.41 g/cm3, respectively. Cyprine is optically uniaxial, negative, ω = 1.744(2), ε= 1.732(2) (in white light). Pleochroism is strong; ranging from O = dark purple, E = pale red to O = dark reddish brown, E = pale yellowish brown; O ≫ E. Chemical composition (electron microprobe, H2O by thermogravimetric analysis (TGA)) of two chemically different zones (zone-1/zone-2, wt.%) is: SiO2 36.98/36.51; Al2O3 14.98/13.70; CaO 36.70/36.18; MgO 3.24/1.10; Mn2O3 2.27/6.04; CuO 2.39/1.86; Fe2O3 0.62/2.50; Cr2O3 0.23/0.04; H2O 3.30/3.30, total 100.71/101.23. The crystal-chemical formulae (based on the FTIR, TGA/differential scanning calorimetry, SREF, WDS and optical spectra) are Ca8.00Ca1.00(Cu0.95Mg0.05)Ʃ1.00Al4.00(Al5.50Mg1.00Mn3+1.19Fe3+0.22Cr0.09)Ʃ8.00([SiO4]9.91[H4O4]0.09)Ʃ10.00[Si2O7]4((OH)9O)9.91 and Ca18.00Ca1.00(Cu0.90Mg0.10)Ʃ1.00(Al3.22Mn3+0.60Fe30.18)Ʃ4.00(Al4.72Mn3+1.20Fe3+1.06Mn2+0.60Mg0.40Cr0.02)Ʃ8.00([SiO4]9.91[H4O4]0.09)Ʃ10.00[Si2O7]4((OH)9O)Ʃ10.00 for zone-1 and zone-2, respectively. Absorption bands in the IR spectrum are 443, 490, 574, 604, 671, 814, 905, 972, 1015, 3354, 3640 cm−1. The polarized optical absorption spectra have two strong absorption bands at 415 and 555 nm and a less intense band at 645 nm. The eight strongest lines of the powder X-ray diffraction pattern are (I–d(Å)–h k l): 12–5.89–002, 12–3.007–431, 47–2.950–004, 100–2.75–432, 76–2.594–522, 35–2.459–620, 10–2.324–144, 28–1.6224–672. Cyprine is tetragonal, space group P4/n, unit-cell parameters refined from the powder data are a = 15.5652(5), c = 11.7921(4), V = 2863.2 (2) Å3,Z = 2. The crystal structure has been refined to R1 = 0.034 and R1 = 0.035 for 2848 and 2071 unique observed reflections with |Fo| ≥ 4σF for the zones 1 and 2, respectively. The structure refinements provide scattering factors of the Y1A,B sites close to 29 e−, which supports occupancy of these sites by Cu2+ ions. The copper coordination polyhedra possess strong Jahn–Teller distortion: Y1A–O6(4×) = 2.043(3) Å and Y1A–O10 = 2.258(6) Å for zone-1 and Y1B–O6(4×) = 2.010(4) Å and Y1B–O10 = 2.274(7) Å for zone-2. Cyprine is defined as a member of the vesuvianite group with Cu2+ as a dominant cation in the Y1 site. The historical name cyprine (derived from Latin cuprum, copper) given by J.J. Berzelius in 1821 for Cu-bearing vesuvianite is transferred to the new mineral.
Skip Nav Destination
Article navigation
Research Article|
May 01, 2017
Cyprine, Ca19Cu2+(Al,Mg,Mn)12Si18O69(OH)9, a new vesuvianite-group mineral from the Wessels mine, South Africa
Taras L. Panikorovskii;
1
Department of Crystallography, Saint-Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, Russia*
Corresponding author, e-mail: [email protected]
Search for other works by this author on:
Vladimir V. Shilovskikh;
Vladimir V. Shilovskikh
2
Department of Colloidal Chemistry, Institute of Chemistry, Saint-Petersburg State University, University Av.26, 198504 St. Petersburg, Russia
Search for other works by this author on:
Evgenia Yu. Avdontseva;
Evgenia Yu. Avdontseva
1
Department of Crystallography, Saint-Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, Russia
Search for other works by this author on:
Andrey A. Zolotarev;
Andrey A. Zolotarev
1
Department of Crystallography, Saint-Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, Russia
Search for other works by this author on:
Igor V. Pekov;
Igor V. Pekov
3
Department of Mineralogy, Moscow State University, Vorobievy Gory, 119991 Moscow, Russia
Search for other works by this author on:
Sergey N. Britvin;
Sergey N. Britvin
1
Department of Crystallography, Saint-Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, Russia
Search for other works by this author on:
Ulf Hålenius;
Ulf Hålenius
4
Department of Geosciences, Swedish Museum of Natural History, Box 50007, 104 05 Stockholm, Sweden
Search for other works by this author on:
Sergey V. Krivovichev
Sergey V. Krivovichev
1
Department of Crystallography, Saint-Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, Russia5
Institute of Silicate Chemistry, Russian Academy of Sciences, Makarova Emb. 6, 199034 St. Petersburg, Russia
Search for other works by this author on:
1
Department of Crystallography, Saint-Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, Russia
Vladimir V. Shilovskikh
2
Department of Colloidal Chemistry, Institute of Chemistry, Saint-Petersburg State University, University Av.26, 198504 St. Petersburg, Russia
Evgenia Yu. Avdontseva
1
Department of Crystallography, Saint-Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, Russia
Andrey A. Zolotarev
1
Department of Crystallography, Saint-Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, Russia
Igor V. Pekov
3
Department of Mineralogy, Moscow State University, Vorobievy Gory, 119991 Moscow, Russia
Sergey N. Britvin
1
Department of Crystallography, Saint-Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, Russia
Ulf Hålenius
4
Department of Geosciences, Swedish Museum of Natural History, Box 50007, 104 05 Stockholm, Sweden
Sergey V. Krivovichev
1
Department of Crystallography, Saint-Petersburg State University, University Emb. 7/9, 199034 St. Petersburg, Russia5
Institute of Silicate Chemistry, Russian Academy of Sciences, Makarova Emb. 6, 199034 St. Petersburg, Russia*
Corresponding author, e-mail: [email protected]
Publisher: Deutsche Mineralogische Gesellschaft, Sociedad Española de Mineralogia, Societá Italiana di Mineralogia e Petrologia, Société Francaise de Minéralogie
Received:
26 May 2016
Revision Received:
18 Aug 2016
Accepted:
19 Aug 2016
First Online:
17 Nov 2017
Online ISSN: 1617-4011
Print ISSN: 0935-1221
© 2017 E. Schweizerbart’sche Verlagsbuchhandlung Science Publishers
E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
European Journal of Mineralogy (2017) 29 (2): 295–306.
Article history
Received:
26 May 2016
Revision Received:
18 Aug 2016
Accepted:
19 Aug 2016
First Online:
17 Nov 2017
Citation
Taras L. Panikorovskii, Vladimir V. Shilovskikh, Evgenia Yu. Avdontseva, Andrey A. Zolotarev, Igor V. Pekov, Sergey N. Britvin, Ulf Hålenius, Sergey V. Krivovichev; Cyprine, Ca19Cu2+(Al,Mg,Mn)12Si18O69(OH)9, a new vesuvianite-group mineral from the Wessels mine, South Africa. European Journal of Mineralogy 2017;; 29 (2): 295–306. doi: https://doi.org/10.1127/ejm/2017/0029-2592
Download citation file:
You could not be signed in. Please check your email address / username and password and try again.
Index Terms/Descriptors
- Africa
- cell dimensions
- chemical composition
- coordination
- copper
- crystal chemistry
- crystal form
- crystal structure
- electron probe data
- formula
- FTIR spectra
- infrared spectra
- metals
- new minerals
- Northern Cape Province South Africa
- optical properties
- orthosilicates
- physical properties
- pleochroism
- refinement
- silicates
- sorosilicates
- South Africa
- Southern Africa
- spectra
- TGA data
- X-ray diffraction data
- Wessels Mine
- differential scanning calorimetry
- Kalahari manganese field
- cyprine
- vesuvianite group
- Hotazel South Africa
Latitude & Longitude
Citing articles via
Related Articles
Delhuyarite-(Ce) – Ce 4 Mg(Fe 3+ 2 W)□(Si 2 O 7 ) 2 O 6 (OH) 2 – a new mineral of the chevkinite group, from the Nya Bastnäs Fe–Cu–REE deposit, Sweden
European Journal of Mineralogy
Cairncrossite, a new Ca-Sr (-Na) phyllosilicate from the Wessels Mine, Kalahari Manganese Field, South Africa
European Journal of Mineralogy
Related Book Content
Aperiodic mineral structures
Mineralogical Crystallography
Variations on the silica theme: Classification and provenance from Pliny to current supplies
The Contribution of Mineralogy to Cultural Heritage
Mineral pigments: the colourful palette of nature
The Contribution of Mineralogy to Cultural Heritage
The relevance of dawsonite precipitation in CO 2 sequestration in the Mihályi-Répcelak area, NW Hungary
Reservoir Quality of Clastic and Carbonate Rocks: Analysis, Modelling and Prediction