Hungchaoite
A valid IMA mineral species
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Formula:
Mg(B4O7) · 9H2O
Colour:
colorless
Lustre:
Vitreous
Hardness:
2½
Specific Gravity:
1.706
Crystal System:
Triclinic
Name:
Named in honor of Chang Hung-chao (章鸿钊) (11 March 1877, Huzhou, Zhejiang Province, China - 6 September 1951, Nanjing, Jiangsu Province, China), geologist, mineralogist, and professor. He is considered one of the founders of modern Chinese geology and was a founder of the Chinese Geological Society.
This mineral has been reported from an undisclosed salt lake on the Qinghai-Tibet plateau (Zhu et al., 1964), a huge area that includes northern Tibet and northwestern Qinghai provinces. According to Yang (1991), Da Qaidam salt lake in Qinghai Province is the only occurrence of the mineral in that area.
Unique Identifiers
Mindat ID:
1950
Long-form identifier:
mindat:1:1:1950:3
IMA Classification of Hungchaoite
Approved
IMA Formula:
MgB4O5(OH)4·7H2O
First published:
1964
Classification of Hungchaoite
6.DA.20
6 : BORATES
D : Tetraborates
A : Neso-tetraborates
6 : BORATES
D : Tetraborates
A : Neso-tetraborates
26.4.3.1
26 : HYDRATED BORATES CONTAINING HYDROXYL OR HALOGEN
4 : Tetraborates
26 : HYDRATED BORATES CONTAINING HYDROXYL OR HALOGEN
4 : Tetraborates
9.2.12
9 : Borates
2 : Borates of Be and Mg
9 : Borates
2 : Borates of Be and Mg
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 for Standard |
|---|---|---|
| Hch | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Hungchaoite
Vitreous
Transparency:
Transparent
Colour:
Colorless
Hardness:
2½ on Mohs scale
Tenacity:
Brittle
Cleavage:
Perfect
{111}, perfect; {111}, good; {010}, imperfect.
{111}, perfect; {111}, good; {010}, imperfect.
Density:
1.706(5) g/cm3 (Measured) 1.703 g/cm3 (Calculated)
Optical Data of Hungchaoite
Type:
Biaxial (-)
RI values:
nα = 1.445(2) nβ = 1.485(2) nγ = 1.490(2)
2V:
Measured: 15° (2), Calculated: 36°
Max. Birefringence:
δ = 0.045
Based on recorded range of RI values above.
Based on recorded range of RI values above.
Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
Surface Relief:
Moderate (negative)
Relative to Canada balsam mounting medium (n ≈ 1.537).
Relative to Canada balsam mounting medium (n ≈ 1.537).
This shows the grain boundary and Becke line effect under plane-polarised
light, based on the contrast between this mineral's average refractive
index and the mounting medium. It does not take into account mineral
colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure
- the conoscopic view for a grain cut perpendicular to the acute bisectrix, using
this mineral's 2V. The two small white dots mark the melatopes - the points
where the two optic axes emerge - and are shown only when they fall within the
field of view. The coloured bands are isochromatics, and the dark bands are
isogyres.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
relatively strong
Chemistry of Hungchaoite
Mindat Formula:
Mg(B4O7) · 9H2O
Element Weights:
Elements listed:
Crystallography of Hungchaoite
Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 8.807(1) Å, b = 10.657(1) Å, c = 7.897(1) Å
α = 103.39(1)°, β = 108.53(1)°, γ = 97.18(1)°
α = 103.39(1)°, β = 108.53(1)°, γ = 97.18(1)°
Ratio:
a:b:c = 0.826 : 1 : 0.741
Unit Cell V:
667.62 ų (Calculated from Unit Cell)
Z:
2
Crystal Structure
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Data courtesy of the American Mineralogist Crystal Structure Database. Click on an AMCSD ID to view structure
| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0000603 | Hungchaoite | Wan C, Ghose S (1977) Hungchaoite, Mg(H2O)5B4O5(OH)4.2H2O: a hydrogen-bonded molecular complex American Mineralogist 62 1135-1143 | ![]() | 1977 | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 6.71 Å | (100) |
| 3.356 Å | (92) |
| 5.36 Å | (85) |
| 4.093 Å | (78) |
| 2.912 Å | (73) |
| 4.079 Å | (64) |
| 7.14 Å | (59) |
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Near-surface Processes | |
| 25 : Evaporites (prebiotic) |
Type Occurrence of Hungchaoite
Geological Setting of Type Material:
saline lacustrine sediments
Associated Minerals at Type Locality:
Other Language Names for Hungchaoite
Dutch:Hungchaoiet
German:Hungchaoit
Russian:Хунчжаоит
Simplified Chinese:章氏硼镁石
Spanish:Hungchaoita
Traditional Chinese:章氏硼鎂石
Related Minerals - Strunz-mindat Grouping
| 6.DA.10 | Borax | Na2(B4O5)(OH)4 · 8H2O |
| 6.DA.15 | Tincalconite | Na2(B4O7) · 5H2O |
| 6.DA.25 | Roweite | Ca2Mn2+2B4O7(OH)6 |
| 6.DA.25 | Fedorovskite | Ca2Mg2B4O7(OH)6 |
| 6.DA.30 | Hydrochlorborite | Ca4B8O15Cl2 · 21H2O |
| 6.DA.35 | Uralborite | Ca2[B3O3(OH)5 · OB(OH)3] |
| 6.DA.40 | Numanoite | Ca4Cu(B4O6(OH)6)(CO3)2 |
| 6.DA.40 | Borcarite | Ca4Mg(B4O6(OH)6)(CO3)2 |
| 6.DA.60 | Fontarnauite | (Na,K)2(Sr,Ca)(SO4)[B5O8(OH)] · 2H2O |
Fluorescence of Hungchaoite
nonfluorescent
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 Hungchaoite
mindat.org URL:
https://www.mindat.org/min-1950.html
Please feel free to link to this page.
Please feel free to link to this page.
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References for Hungchaoite
Reference List:
IMA (1967) International Mineralogical Association: Commission on New Minerals and Mineral Names. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (277) 131-136 doi:10.1180/minmag.1967.036.277.20
Wan, Che'ng, Ghose, Subrata (1977) Hungchaoite, Mg(H2O)5B4O5(OH)4·2H2O: a hydrogen bonded molecular complex. American Mineralogist, 62 (11-12) 1135-1143
Erd, Richard C., McAllister, James F., Eberlein, G. Donald (1979) New data on hungchaoite, the second world occurrence, Death Valley region, California. American Mineralogist, 64 (3-4) 369-375
Localities for Hungchaoite
Showing 7 localities.
Locality List
- 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).
All localities listed without proper references should be considered as questionable.
China (TL) | |
| Yihua Zhu et al. (1964) +3 other references |
Kazakhstan | |
| Anatoly Kasatkin data |
Romania | |
| HÎRTOPANU et al. (2025) |
USA | |
| Erd et al. (1970) +2 other references |
| Erd et al. (1979) +2 other references |
| Erd et al. (1979) | |
| Erd et al. (1979) +2 other references |
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