Diaoyudaoite
Chemical formula: NaAl<sub>11</sub>O<sub>17</sub>
Diaoyudaoite is an extremely rare sodium aluminum oxide, occurring as microscopic, hexagonal platelets in meteorites.
Properties
- Mohs hardness
- 7.5-8
- Luster
- Vitreous
- Streak
- White
- Cleavage
- Perfect on {0001}
- Transparency
- Transparent
- Crystal system
- Hexagonal
Diagnostic features
## Identification Identification of diaoyudaoite is only possible using advanced laboratory techniques, such as scanning electron microscopy (SEM) with chemical composition analysis (EDS) and X-ray diffraction (XRD). In collector or field conditions, identification is impossible. It is observed as fine, hexagonal platelets in calcium-aluminum-rich inclusions (CAIs) within meteorites. ## Distinguishing from similar minerals Diaoyudaoite is closely related to hibonite, with which it forms a solid solution. Distinguishing these two minerals requires precise chemical analysis to determine the ratio of sodium to calcium and rare earth elements. Visually, without analysis, they are indistinguishable. ## Crystal forms It forms exclusively microscopic, hexagonal, tabular or platy crystals.
Geological environment
## Genesis Diaoyudaoite is an extraterrestrial mineral. It forms in the very early stages of Solar System formation at high temperatures, as one of the components of calcium-aluminum-rich inclusions (CAIs) in carbonaceous chondrites. It is believed to have condensed directly from the solar nebula. ## Mineral associations It most commonly co-occurs with other minerals forming in CAIs, such as hibonite, perovskite, spinel, and melilite. These minerals represent some of the oldest solids formed in our Solar System. ## Localities Its occurrence has been confirmed in several meteorites. The type locality (holotype) is the Allende meteorite, which fell in Chihuahua, Mexico. It has also been found in the Murchison meteorite (Australia), Acfer 094 (Algeria), and NWA 529 (Northwest Africa).
Rarity
Extremely rare
For collectors
## Quality criteria For such a rare microscopic mineral, the primary criterion for value is the confirmed presence of diaoyudaoite in the meteorite sample itself. Higher quality specimens are those in which the crystals are relatively "large" (tens of micrometers), well-formed, and occur in rich concentrations. Scientific documentation confirming the mineral's identification is crucial. ## Popular localities The most known and classic source of diaoyudaoite specimens is the Allende meteorite. Samples from this fall are most sought after by specialized collectors of meteoritic minerals.
Care and storage
## Cleaning Specimens containing diaoyudaoite, due to their microscopic nature and embedding in the meteorite matrix, generally do not require and should not be subjected to cleaning. Any attempt at mechanical or chemical cleaning risks irreversible damage or loss of the microscopic crystals. ## What to avoid Avoid all chemicals, ultrasonics, and changes in temperature and humidity. Meteorite specimens can be sensitive to atmospheric conditions, so they should be protected from moisture, which could cause corrosion of the surrounding matrix. ## Storage Diaoyudaoite samples should be stored under stable conditions, preferably in closed, padded "micromount" boxes or in humidity-controlled containers. Protect from dust and direct sunlight.