Cubo-ice
A valid IMA mineral species
This page is currently not sponsored. Click here to sponsor this page.
Formula:
H2O
Crystal System:
Isometric
Name:
Long known as a synthetic material under the name ice-VII. That name was kept after the discovery of natural material. The name was changed by the IMA to cubo-ice in 2022.
Type Locality:
Dimorph of:
Cubo-ice is better known as ice-VII.
Found as inclusion in a diamond from Orapa, Botswana.
Cubo-ice is structurally closely related to cuprite Cu2O.
Found as inclusion in a diamond from Orapa, Botswana.
Cubo-ice is structurally closely related to cuprite Cu2O.
Unique Identifiers
Mindat ID:
51969
Long-form identifier:
mindat:1:1:51969:2
GUID
(UUID V4):
(UUID V4):
2d3f1d74-ef57-45c3-858c-2377a4e78113
IMA Classification of Cubo-ice
Classification of Cubo-ice
4.AA.10
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
A : Metal: Oxygen = 2:1 and 1:1
A : Cation:Anion (M:O) = 2:1 (and 1.8:1)
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
A : Metal: Oxygen = 2:1 and 1:1
A : Cation:Anion (M:O) = 2:1 (and 1.8:1)
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Symbol | Source | Reference |
---|---|---|
Ice-VII | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Chemistry of Cubo-ice
Mindat Formula:
H2O
Elements listed:
Crystallography of Cubo-ice
Crystal System:
Isometric
Cell Parameters:
a = 3.1633(3) Å
Unit Cell V:
31.65 ų (Calculated from Unit Cell)
Comment:
Spacegroup: Pn-3m
X-Ray Powder Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
2.237 Ã… | (100) |
1.582 Ã… | (11) |
1.291 Ã… | (23) |
1.118 Ã… | (7) |
1.000 Ã… | (7) |
0.913 Ã… | (2) |
0.845 Ã… | (8) |
0.791 Ã… | (1) |
Comments:
From Type Description.
Geological Environment
Paragenetic Mode(s):
Paragenetic Mode | Earliest Age (Ga) |
---|---|
Stage 4b: Highly evolved igneous rocks | >3.0 |
36 : Carbonatites, kimberlites, and related igneous rocks |
Type Occurrence of Cubo-ice
Place of Conservation of Type Material:
Type material is deposited in the mineralogical collections of the Royal Ontario Museum, Toronto, Ontario, Canada, accession number M57666.
Geological Setting of Type Material:
An inclusion in diamond formed at a pressure of 11 GPa.
Associated Minerals at Type Locality:
Synonyms of Cubo-ice
Related Minerals - Strunz-mindat Grouping
4.AA.05 | Ice | H2O |
4.AA.10 | Cuprite | Cu2O |
4.AA.15 | Paramelaconite | Cu1+2Cu2+2O3 |
Other Information
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Internet Links for Cubo-ice
mindat.org URL:
https://www.mindat.org/min-51969.html
Please feel free to link to this page.
Please feel free to link to this page.
Search Engines:
External Links:
Mineral Dealers:
References for Cubo-ice
Reference List:
HÃ¥lenius, U., Hatert, F., Pasero, M., Mills, S. J. (2017) New minerals and nomenclature modifications approved in 2017, CNMNC Newsletter No 38. Mineralogical Magazine, 81 (4) 1033-1038 doi:10.1180/minmag.2017.081.062
Localities for Cubo-ice
ⓘ - Click for references and further information on this occurrence.
? - Indicates mineral may be doubtful at this locality.
- Good crystals or important locality for species.
- World class for species or very significant.
(TL) - Type Locality for a valid mineral species.
(FRL) - First Recorded Locality for everything else (eg varieties).
Struck out - Mineral was erroneously reported from this locality.
Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).
All localities listed without proper references should be considered as questionable.
All localities listed without proper references should be considered as questionable.
Botswana (TL) | |
| HÃ¥lenius et al. (2017) +2 other references |
China | |
Tschauner et al. (2018) | |
South Africa | |
| Tschauner et al. (2018) |