F. Bernhard et al., PRETULITE, SCPO4, A NEW SCANDIUM MINERAL FROM THE STYRIAN AND LOWER AUSTRIAN LAZULITE OCCURRENCES, AUSTRIA, The American mineralogist, 83(5-6), 1998, pp. 625-630
Pretulite is a new Sc phosphate with zircon-type structure from the ph
yllite-micaschist hosted hydrothermal lazulite-quartz veins in the Low
er Austroalpine Grobgneis complex, eastern Austria. The new species is
the Sc-dominant analogue of xenotime-(Y) and occurs as an accessory m
ineral in all investigated lazulite specimens, forming anhedral to euh
edral crystals up to 200 mu m long with the dominant form {211}. It is
associated with lazulite, fluorapatite, chlorapatite, quartz, muscovi
te, clinochlore, paragonite, kyanite, pyrophyllite, augelite, wardite,
hydroxylherderite, goyazite, florencite-(Ce), xenotime-(Y), bearthite
, rutile, pyrite, corundum, and an AlO(OH)-phase. Pretulite is translu
cent to transparent with an adamantine luster, colorless to pale pink,
uniaxial positive with omega = 1.790 (5), epsilon = 1.86 (1) and show
s a weak orange fluorescence at 254 nm as well, as a bright blue catho
doluminescence. Mohs hardness is about 5. The empirical formula for pr
etulite (based on four O atoms) is (Sc0.98Y0.02)(1.00)P1.00O4.00. It c
ontains variable amounts of Y with Y/(Y + Sc) = 0.5 - 3.2 mol% and tra
ces of Yb, Er, and Dy. The space group is I4(1)/amd with a = 6.589 (1)
Angstrom, c = 5.806 (1) Angstrom, V = 252.1 (1) Angstrom(3), d(calc)
= 3.71 g/cm(3), Z = 4. The four strongest lines in the X-ray powder pa
ttern are d(200) = 3.293 (100), d(112) = 2.4636 (42), d(312) = 1.6927
(45), d(332) = 1.3697 (15) Angstrom. The crystal structure was refined
using 108 reflections to R(F-0) = 0.018. Cell parameters and average
M-O distances confirm a small amount of Y substituting Sc in the eight
fold-coordinated M-position. The formation of pretulite is attributed
to a moderate enrichment of Sc in lazulite-rich domains of the veins (
about 180 ppm) and the inability of the accompanying minerals to incor
porate larger quantities of Sc in their crystal structure. The name is
after the mountain Pretul, Fischbacher Alpen, Styria, Austria.