| Lulzacite | |
|---|---|
|   Lulzacite found in France | |
| General | |
| Category | Phosphate minerals | 
| Formula | Sr2Fe2+(Fe2+,Mg)2Al4(PO4)4(OH)10 | 
| IMA symbol | Lul [1] | 
| Strunz classification | 8.BK.25 | 
| Crystal system | Triclinic | 
| Crystal class | Pinacoidal (1) (same H-M symbol) | 
| Space group | P1 | 
| Identification | |
| Color | Grayish-green to yellowish-green | 
| Crystal habit | Anhedral aggregates; rarely small euhedral crystals | 
| Cleavage | None | 
| Mohs scale hardness | 5.5–6 | 
| Luster | Vitreous | 
| Diaphaneity | Transparent–translucent | 
| Specific gravity | 3.55 | 
| Optical properties | Biaxial (−) | 
| Refractive index | nα = 1.654 nβ = 1.674 nγ = 1.684 | 
| Birefringence | δ = 0.030 | 
| References | [2] [3] [4] | 
Lulzacite is a strontium-containing phosphate mineral with the chemical formula Sr2Fe2+(Fe2+,Mg)2Al4(PO4)4(OH)10. [2] [3]
The mineral was first described in 2000 from quartzite deposits ( 47°42′50″N1°29′20″W / 47.71389°N 1.48889°W ) at Saint-Aubin-des-Châteaux, Loire-Atlantique, France, and is named after Y. Lulzac, a French geologist who discovered the mineral. In this deposit, lulzacite occurs within quartz and siderite veinlets at quartzite–limestone contacts. Other minerals found in the veinlets include apatite, goyazite, and pyrite. [4]
Lulzacite crystallizes in the triclinic system with P1 space group. It is isostructural with jamesite (Pb2Zn(Fe2+,Zn)2Fe3+4(AsO4)4(OH)10). [4] [5]