Khmaralite was found in "Zircon Point" on Khmara Bay, Enderby Land, Antarctica and occurs in a metamorphosed pegmatite. It is named after the area that it was found, which was named in the honor of Ivan Fedorovich Khmara who was a tractor driver that died in Antarctica.^[2][3][4]

The associated minerals with khamralite (sillimanite, surinamite, musgravite, garnet, and biotite) saturated it in BeO, allowing the BeO content to be close to the maximum possible. This is a rare instance, and has not been located elsewhere.^[4]

Barbier et al. analyzed khmaralite for constituents other than Li, Be and B with an ARL-EMX electron microprobe using 15 kV accelerating voltage and a 20 nA sample current. Li, Be and B were analyzed with an ARL Ion Microprobe Mass Analyzer (IMMA). It was later found in 1996 while using a Camea ims 4f (Secondary Ion Mass Spectroscopy or SIMS) that the ⁹Be⁺ signal was not corrected for the ²⁷Al⁺ signal in the IMMA data. The IMMA and SIMS BeO contents are respectively, 2.56 and 2.47 weight percent.^[4]

(*Fe was analyzed as Fe²⁺; FeO and Fe₂O₃ were calculated assuming 28 cations in a formula for 40 O atoms.) ^[4]

Khmaralite has a superstructure that is best described as a doubled sapphirine unit cell because the a axis is in the direction of the tetrahedral chains along which the main cation ordering occurs.^[4]

There are rows of weak extra reflections that correspond to a doubling of the a axis. These patterns are indexed by the unit cell (P2₁/c): a = 19.8, b = 14.4, c = 11.2 Å, β = 125°. These were found using electron diffraction and microscopy. The superstructure was also observed in a medium-resolution lattice along the [001] axis. There was also a slight comparison made between the superstructure and the thicker regions of the crystals corresponding to a double₁₀₀ interplanar spacing equal to 16.1 Å.^[4]

The powdered x-ray diffraction pattern had a slightly different conclusion but relatively the same as the electron diffraction and microscopy end numbers. The powder pattern was indexed on a monoclinic unit cell and the absences consistent with the P2₁/c space group were found. The unit cell was similar to the electron diffraction and microscopy: a = 19.794(8), b = 14.367(5), c = 11.320(3) Å, β = 125.49(4)°. But there was an unexplained 0.066 Å difference in the c parameters. The reflections that correspond to the 2xa superstructure are not visible in the powder x-ray pattern of khmaralite. The intensity of the strongest super-cell reflection is only 0.4% of that of the most intense sub-cell reflection.^[4]

These experiments were then refined, and corrected displaying the notable 2xa superstructure of khmaralite.^[4]

The major differences between khmaralite and sapphirine-2M are the presence of a 2xa superstructure and the larger count of Be at one tetrahedral site. Khmaralite and sapphirine-2M cannot be distinguished by optical properties alone because the internal effects of Be on the crystal structure are covered by the effect of Fe substitution for Mg and Al. But the presence of 2 wt% or more of BeO indicates a likely advocate for khmaralite. Confirmation is available by using electron diffraction to see if there is a presence of a superstructure.^[4]

Article on Khmaralite, From American Mineralogist