Nanlingite (original) (raw)
4.JB.25
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
B : Arsenites, antimonites, bismuthites; with additional anions, without H2O
46.1.2.1
46 : ANTIMONITES AND ARSENITES CONTAINING HYDROXYL OR HALOGEN
1 : (AB)m(XO3)pZq
Colour:
Brownish red to dark brown when oxidized
Hardness:
VHN100=107 - Vickers
Density:
3.927 g/cm3 (Measured) 3.925 g/cm3 (Calculated)
Class (H-M):
3_m_ _(_32/m ) - Hexagonal Scalenohedral
Cell Parameters:
a = 10.2114(10) Å, c = 25.689(3) Å
Unit Cell V:
2,319.79 ų (Calculated from Unit Cell)
Morphology:
Tabular, with {0001} and {h0hl}.
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0018326 | Nanlingite | Yang Z, Giester G, Ding K, Tillmanns E (2011) Crystal structure of nanlingite - the first mineral with a [Fe(AsO3)6] configuration European Journal of Mineralogy 23 63-71 | 2011 | Nanling area, Hunan Province, China | 0 | 293 |
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Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The
symbol next to localities in the list can be used to jump to that position on the map.
- This locality has map coordinates listed.
- This locality has estimated coordinates. ⓘ - 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.
China (TL) | |
---|---|
Hunan Chenzhou Yizhang Co. Dongpo ore field ⓘ Shizhuyuan Mine (TL) | Gu Xiongfei et al. (1976) |