Anzaite-(Ce) | |
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General | |
Category | Oxide mineral |
Formula (repeating unit) | Ce4Fe2+Ti6O18(OH)2 |
IMA symbol | Anz-Ce[1] |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | C2/m |
Unit cell | a = 5.29, b = 14.58 c = 5.23 [Å]; β = 97.23° (approximated); Z = 1 |
Identification | |
Color | Grey |
Crystal habit | Crystals (tiny) |
Cleavage | None |
Tenacity | Brittle |
Mohs scale hardness | 6–6.5 |
Diaphaneity | Opaque |
Density | 5.05 (calculated; approximated) |
References | [2][3] |
Anzaite-(Ce) is a rare-earth element (REE) oxide mineral with the formula Ce4Fe2+Ti6O18(OH)2.[2][3] An example of chemically related mineral is lucasite-(Ce),[4] although it contains no iron. Cerium in anzaite-(Ce) is mainly substituted by neodymium, lanthanum, calcium and praseodymium. Titanium is substituted by niobium. Trace elements include thorium. The mineral is monoclinic, space group C2/m. Anzaite-(Ce) is hydrothermal mineral found in a carbonatite from the mineralogically prolific Kola Peninsula. The mineral name honors Anatoly N. Zaitsev, who is known for studies of carbonatites and REE.[2][3]
Parent rocks for anzaite-(Ce) are silicocarbonatites of the Afrikanda alkali-ultramafic massif. These rocks underwent hydrothermal reworking, that beside anzaite-(Ce) produced also calcite, clinochlore, hibschite and titanite in expense of primary minerals.[2]
Cerium in anzaite-(Ce) is substituted by significant amounts of neodymium, lanthanum, calcium, and praseodymium, with minor samarium and thorium. Other impurities in the mineral composition include niobium and silicon.
The crystal structure of anzaite-(Ce) characterizes in:[2]
The disordered sites are located on the (010) planes, separated by ordered domains containing REE, VITi (octahedral) and two oxide-anion sites.[2]