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Hungchaoite

A valid IMA mineral species
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05174500017271923831707.jpg
Chang Hung-chao
Formula:
Mg(B4O7) · 9H2O
Colour:
colorless
Lustre:
Vitreous
Hardness:
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.


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Unique IdentifiersHide

Mindat ID:
1950
Long-form identifier:
mindat:1:1:1950:3

IMA Classification of HungchaoiteHide

Classification of HungchaoiteHide

6.DA.20

6 : BORATES
D : Tetraborates
A : Neso-tetraborates
26.4.3.1

26 : HYDRATED BORATES CONTAINING HYDROXYL OR HALOGEN
4 : Tetraborates
9.2.12

9 : Borates
2 : Borates of Be and Mg

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
HchIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of HungchaoiteHide

Vitreous
Transparency:
Transparent
Colour:
Colorless
Hardness:
2½ on Mohs scale
Tenacity:
Brittle
Cleavage:
Perfect
{111}, perfect; {111}, good; {010}, imperfect.
Density:
1.706(5) g/cm3 (Measured)    1.703 g/cm3 (Calculated)

Optical Data of HungchaoiteHide

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.

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.

Surface Relief:
Moderate (negative)
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.
Dispersion:
relatively strong

Chemistry of HungchaoiteHide

Mindat Formula:
Mg(B4O7) · 9H2O
Element Weights:
Element% weight
O74.921 %
B12.656 %
Mg7.113 %
H5.310 %

Calculated from ideal end-member formula.
O
B
Mg
H

Crystallography of HungchaoiteHide

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)°
Ratio:
a:b:c = 0.826 : 1 : 0.741
Unit Cell V:
667.62 ų (Calculated from Unit Cell)
Z:
2

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0000603HungchaoiteWan C, Ghose S (1977) Hungchaoite, Mg(H2O)5B4O5(OH)4.2H2O: a hydrogen-bonded molecular complex American Mineralogist 62 1135-114319770293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
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 EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
25 : Evaporites (prebiotic)

Type Occurrence of HungchaoiteHide

Other Language Names for HungchaoiteHide

German:Hungchaoit
Simplified Chinese:章氏硼镁石
Spanish:Hungchaoita
Traditional Chinese:章氏硼鎂石

Related Minerals - Strunz-mindat GroupingHide

6.DA.10BoraxNa2(B4O5)(OH)4 · 8H2OMon. 2/m : B2/b
6.DA.15TincalconiteNa2(B4O7) · 5H2OTrig. 32 : R32
6.DA.25RoweiteCa2Mn2+2B4O7(OH)6Orth. mmm(2/m2/m2/m) : Pbam
6.DA.25FedorovskiteCa2Mg2B4O7(OH)6Orth. mmm(2/m2/m2/m) : Pbam
6.DA.30HydrochlorboriteCa4B8O15Cl2 · 21H2OMon. 2/m
6.DA.35UralboriteCa2[B3O3(OH)5 · OB(OH)3]Mon. 2/m
6.DA.40NumanoiteCa4Cu(B4O6(OH)6)(CO3)2Mon. 2/m : B2/m
6.DA.40BorcariteCa4Mg(B4O6(OH)6)(CO3)2Mon. 2/m : B2/m
6.DA.60Fontarnauite(Na,K)2(Sr,Ca)(SO4)[B5O8(OH)] · 2H2OMon. 2/m : P21/b

Fluorescence of HungchaoiteHide

nonfluorescent

Other InformationHide

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 HungchaoiteHide

References for HungchaoiteHide

Reference List:

Localities for HungchaoiteHide

Showing 7 localities.

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.
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Locality ListHide

- 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)
 
  • Qinghai
    • Haixi Mongol and Tibetan Autonomous Prefecture
      • Da Qaidam (Dachaidan Co.)
Yihua Zhu et al. (1964) +3 other references
Kazakhstan
 
  • Atyrau Region
    • Inder District
Anatoly Kasatkin data
Romania
 
  • Maramureș County
    • Târgu Lăpuș
HÎRTOPANU et al. (2025)
USA
 
  • California
    • Inyo County
      • Furnace Creek Mining District (Furnace Creek Borate Mining District)
        • Ryan
Erd et al. (1970) +2 other references
        • Twenty Mule Team Canyon
Erd et al. (1979) +2 other references
Erd et al. (1979)
Erd et al. (1979) +2 other references
 
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