Khmaralite
A valid IMA mineral species
This page is currently not sponsored. Click here to sponsor this page.
About Khmaralite
Formula:
(Mg,Al,Fe)16[(Al,Si,Be)12O36]O4
Colour:
Dark greenish blue to very dark green
Lustre:
Vitreous
Hardness:
7
Specific Gravity:
3.61 (Calculated)
Crystal System:
Monoclinic
Member of:
Name:
For the locality, Khmara Bay, Antartica, which in turn was named in honor of Ivan Fedorovich Khmara (1936-1956), a tractor driver who perished in Antarctica.
Unique Identifiers
Mindat ID:
7136
Long-form identifier:
mindat:1:1:7136:5
IMA Classification of Khmaralite
Classification of Khmaralite
9.DH.50
9 : SILICATES (Germanates)
D : Inosilicates
H : Inosilicates with 4-periodic single chains, Si4O12
9 : SILICATES (Germanates)
D : Inosilicates
H : Inosilicates with 4-periodic single chains, Si4O12
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 |
|---|---|---|
| Kma | 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 Khmaralite
Vitreous
Transparency:
Translucent
Colour:
Dark greenish blue to very dark green
Streak:
Green-gray
Hardness:
7 on Mohs scale
Tenacity:
Brittle
Cleavage:
None Observed
Fracture:
Irregular/Uneven
Density:
3.61 g/cm3 (Calculated)
Optical Data of Khmaralite
Type:
Biaxial (-)
RI values:
nα = 1.725 nβ = 1.740 nγ = 1.741
2V:
Measured: 34° , Calculated: 28°
Birefringence:
0.016
Max. Birefringence:
δ = 0.016
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:
Very High (positive)
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:
r > v strong
Optical Extinction:
Y // b.
Pleochroism:
Strong
Comments:
X = colorless or very light tan, Y = blue-green, and Z = deep blue-green.
Comments:
Very like sapphirine.
Chemistry of Khmaralite
Mindat Formula:
(Mg,Al,Fe)16[(Al,Si,Be)12O36]O4
Element Weights:
Crystallography of Khmaralite
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/b
Cell Parameters:
a = 18.8 Å, b = 14.371 Å, c = 11.254 Å
β = 125.53°
β = 125.53°
Ratio:
a:b:c = 1.308 : 1 : 0.783
Unit Cell V:
2,474.43 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Tablets flattened parallel to {010}.
Comment:
Related to sapphirine-2M but with different cation ordering and doubled chain repeat.
Crystal Structure
Load
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Show
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
Remove metal-metal sticks
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
Remove metal-metal sticks
Display Options
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
View
CIF File Best | x | y | z | a | b | c
CIF File Best | x | y | z | a | b | c
Rotation
Stop | Start
Stop | Start
Labels
Console Off | On | Grey | Yellow
Console Off | On | Grey | Yellow
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) |
|---|---|---|---|---|---|---|---|
| 0002331 | Khmaralite | Barbier J, Grew E S, Moore P B, Su S-C (1999) Khmaralite, a new beryllium-bearing mineral related to sapphirine: A superstructure resulting from partial ordering of Be, Al and Si on tetrahedral sites American Mineralogist 84 1650-1660 | ![]() | 1999 | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 7.7321 Å | (6) |
| 7.1859 Å | (2) |
| 5.3655 Å | (2) |
| 4.4217 Å | (3) |
| 4.1150 Å | (2) |
| 4.0336 Å | (6) |
| 3.5906 Å | (5) |
| 3.2643 Å | (13) |
| 3.2151 Å | (2) |
| 3.0817 Å | (7) |
| 2.9974 Å | (5) |
| 2.9852 Å | (38) |
| 2.9615 Å | (2) |
| 2.8341 Å | (30) |
| 2.8260 Å | (45) |
| 2.7598 Å | (20) |
| 2.7407 Å | (2) |
| 2.7169 Å | (5) |
| 2.6850 Å | (5) |
| 2.6691 Å | (3) |
| 2.6408 Å | (16) |
| 2.6240 Å | (12) |
| 2.5990 Å | (5) |
| 2.5745 Å | (8) |
| 2.5659 Å | (36) |
| 2.5153 Å | (8) |
| 2.4804 Å | (4) |
| 2.4446 Å | (100) |
| 2.4387 Å | (44) |
| 2.4316 Å | (2) |
| 2.4261 Å | (6) |
| 2.4111 Å | (5) |
| 2.3948 Å | (4) |
| 2.3756 Å | (15) |
| 2.3405 Å | (43) |
| 2.3312 Å | (3) |
| 2.3138 Å | (3) |
| 2.2892 Å | (2) |
| 2.2349 Å | (7) |
| 2.2110 Å | (2) |
| 2.1511 Å | (3) |
| 2.1289 Å | (3) |
| 2.1235 Å | (11) |
| 2.0657 Å | (5) |
| 2.0453 Å | (3) |
| 2.0140 Å | (61) |
| 2.0106 Å | (85) |
| 2.0034 Å | (2) |
| 1.9515 Å | (2) |
| 1.9392 Å | (3) |
| 1.8914 Å | (29) |
| 1.8874 Å | (3) |
Comments:
Barbier, J., Grew, E.S., Moore, P.B., and Su, S.-C. (1999) American Mineralogist, 84, 1650–1660.
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 4b: Highly evolved igneous rocks | >3.0 |
| 34 : Complex granite pegmatites |
Type Occurrence of Khmaralite
General Appearance of Type Material:
Foliated aggregates nearly 3 cm across of parallel tablets. The tablets are flattened parallel to {010} and range from 1-7 mm across and from 0.5-4 mm thick.
Place of Conservation of Type Material:
National Museum of Natural History, Washington, D.C., USA, NMNH 171532.
Geological Setting of Type Material:
Pegmatite.
Associated Minerals at Type Locality:
Synonyms of Khmaralite
Other Language Names for Khmaralite
Relationship of Khmaralite to other Species
Member of:
Other Members of Sapphirine Group:
| Addibischoffite | Ca2Al6Al6O20 | Tric. 1 : P1 |
| Louisfuchsite | Ca2(Mg4Ti2)(Al4Si2)O20 | Tric. 1 : P1 |
| Sapphirine | Mg4(Mg3Al9)O4[Si3Al9O36] | Mon. 2/m : P21/b |
| 'UM2002-52-SiO:AlFeMg' | Mg4(Mg1.5Fe+20.3Fe+31.6Al8.5)O4[Si1.7Al10.3O36] | |
| Warkite | Ca2Sc6Al6O20 | Tric. 1 : P1 |
Common Associates
Associations Based on Photo Data:
| 3 photos of Khmaralite associated with Surinamite | (Mg,Fe)3Al4BeSi3O16 |
| 1 photo of Khmaralite associated with Quartz | SiO2 |
Related Minerals - Strunz-mindat Grouping
| 9.DH. | Devilliersite | Ca4Ca2Fe3+10O4[(Fe3+10Si2)O36] |
| 9.DH. | 'Gageite-2M' | (Mn,Mg,Zn)42Si16O54(OH)40 |
| 9.DH. | Bavsiite | Ba2V2O2[Si4O12] |
| 9.DH. | Yuzuxiangite | Sr3Fe3+(Si2O6)2(OH) · 3H2O |
| 9.DH. | Louisfuchsite | Ca2(Mg4Ti2)(Al4Si2)O20 |
| 9.DH.05 | Leucophanite | NaCaBeSi2O6F |
| 9.DH.10 | Ohmilite | Sr3(Ti,Fe3+)(Si4O12)(O,OH) · 2-3H2O |
| 9.DH.15 | Haradaite | SrVSi2O7 |
| 9.DH.15 | Suzukiite | BaVSi2O7 |
| 9.DH.20 | Shcherbakovite | (K,Ba)KNa(Ti,Nb)2(Si4O12)O2 |
| 9.DH.20 | Batisite | BaNaNaTi2(Si4O12)O2 |
| 9.DH.20 | Noonkanbahite | BaKNaTi2(Si4O12)O2 |
| 9.DH.25 | Taikanite | Sr3BaMn2+2(Si4O12)O2 |
| 9.DH.30 | Krauskopfite | BaSi2O5 · 3H2O |
| 9.DH.35 | Gageite | Mn21(Si4O12)2O3(OH)20 |
| 9.DH.35 | Balangeroite | (Mg,Fe2+,Fe3+,Mn2+)42Si16O54(OH)40 |
| 9.DH.40 | Kuratite | Ca2(Fe2+5Ti)O2[Si4Al2O18] |
| 9.DH.40 | Aenigmatite | Na4[Fe2+10Ti2]O4[Si12O36] |
| 9.DH.40 | Dorrite | Ca4(Mg3Fe3+9)O4(Si3Al8Fe3+O36) |
| 9.DH.40 | Serendibite | Ca4[Mg6Al6]O4[Si6B3Al3O36] |
| 9.DH.40 | Rhönite | Ca4[Mg8Fe3+2Ti2]O4[Si6Al6O36] |
| 9.DH.40 | Khesinite | Ca4(Mg3Fe3+9)O4(Fe3+9Si3)O36 |
| 9.DH.40 | 'UM1991-29-SiO:FeMgNa' | Na4(Mg5Fe3+7)O4[Si9Fe3+3O36] |
| 9.DH.40 | Høgtuvaite | Ca4[Fe2+6Fe3+6]O4[Si8Be2Al2O36] |
| 9.DH.40 | 'Leucorhönite' | Ca2(Mg,Fe3+,Al)6(Si,Al)6O20 |
| 9.DH.40 | Welshite | Ca4Mg9Sb3O4[Si6Be3AlFe2O36] |
| 9.DH.40 | Wilkinsonite | Na2Fe2+4Fe3+2(Si6O18)O2 |
| 9.DH.40 | Krinovite | Na2Mg4Cr3+2(Si6O18)O2 |
| 9.DH.40 | Makarochkinite | (Ca,Na)4[Fe2+8Fe3+2Ti2]O4[Si8Be2Al2O36] |
| 9.DH.45 | Sapphirine | Mg4(Mg3Al9)O4[Si3Al9O36] |
| 9.DH.55 | 'UM1988-26-SiO:AlMg' | Mg4Al2O[Si3Al2O15] |
| 9.DH.55 | Surinamite | (Mg,Fe)3Al4BeSi3O16 |
| 9.DH.60 | Deerite | Fe2+6Fe3+3(Si6O17)O3(OH)5 |
| 9.DH.65 | Taneyamalite | (Na,Ca)Mn2+12(Si,Al)12(O,OH)44 |
| 9.DH.65 | Howieite | Na(Fe2+,Fe3+,Al,Mg)12(Si6O17)2(O,OH)10 |
| 9.DH.70 | Johninnesite | Na2Mn2+9Mg7(OH)8[AsO4]2[Si6O17]2 |
| 9.DH.75 | Agrellite | NaCa2Si4O10F |
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 Khmaralite
mindat.org URL:
https://www.mindat.org/min-7136.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 Khmaralite
Reference List:
Grew, Edward S. (1981) Surinamite, taaffeite, and beryllian sapphirine from pegmatites in granulite facies rocks of Casey Bay, Enderby Land, Antarctica. American Mineralogist, 66 (9-10) 1022-1033
Barbier, Jacques, Grew, Edward S., Moore, Paulus B., Su, Shu-Chun (1999) Khmaralite, a new beryllium-bearing mineral related to sapphirine; a superstructure resulting from partial ordering of Be, Al, and Si on tetrahedral sites. American Mineralogist, 84 (10) 1650-1660 doi:10.2138/am-1999-1020
Christy, A.G., Tabira, Y., Hölscher, A., Grew, E.S., Schreyer, W. (2002) Synthesis of beryllian sapphirine in the system MgO-BeO-Al2O3-SiO2-H2O and comparison with naturally occurring beryllian sapphirine and khmaralite. Part 1: Experiments, TEM, and XRD. American Mineralogist, 87 (8) 1104-1112 doi:10.2138/am-2002-8-907
Christy, A.G., Grew, E.S. (2004) Synthesis of beryllian sapphirine in the system MgO-BeO-Al2O3-SiO2-H2O and comparison with naturally occurring beryllian sapphirine and khmaralite, Part 2: A chemographic study of Be content as a function of P, T, assemblage and FeMg–1 exchange. American Mineralogist, 89 (2-3). 327-338 doi:10.2138/am-2004-2-311
Localities for Khmaralite
Showing 4 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.
Antarctica | |
| gsa.confex.com (n.d.) |
| Grew et al. (2000) |
| Grew (1981) +2 other references | |
| Grew et al. (2000) |
Quick NavTopAbout KhmaraliteUnique IdentifiersIMA Classification Classification Mineral SymbolsPhysical Properties Optical Data Chemistry Crystallography Crystal StructureX-Ray Powder DiffractionGeological EnvironmentType Occurrence SynonymsOther LanguagesRelationshipsCommon AssociatesStrunz-MindatOther InformationInternet Links References Localities Locality List



symbol to view information about a locality.
The
"Zircon Point" pegmatite, Khmara Bay, Casey Bay, Napier Complex, Enderby Land, East Antarctica, Antarctica