Lulzacite | |
Category: | Phosphate minerals |
Formula: | Sr2Fe2+(Fe2+,Mg)2Al4(PO4)4(OH)10 |
Imasymbol: | Lul[1] |
Strunz: | 8.BK.25 |
System: | Triclinic |
Class: | Pinacoidal (same H-M symbol) |
Symmetry: | P |
Color: | Grayish-green to yellowish-green |
Habit: | Anhedral aggregates; rarely small euhedral crystals |
Cleavage: | None |
Mohs: | 5.5–6 |
Luster: | Vitreous |
Refractive: | nα = 1.654 nβ = 1.674 nγ = 1.684 |
Opticalprop: | Biaxial (-) |
Birefringence: | δ = 0.030 |
Gravity: | 3.55 |
Diaphaneity: | Transparent–translucent |
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 (47.7139°N -1.4889°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 P space group. It is isostructural with jamesite (Pb2Zn(Fe2+,Zn)2Fe3+4(AsO4)4(OH)10).[4] [5]