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Formula: (CaSm)(AlAlFe2+)O[Si2O7][SiO4](OH)
(Mindat formula)
Sorosilicate (Si2O7 groups), allanite group,
epidote supergroup,
samarium-bearing mineral
Crystal System: Monoclinic
Specific gravity: 3.842 calculated
Hardness: 5
Streak: White
Colour: Yellowish brown
Environments
Pegmatites
Hydrothermal environments
Allanite-(Sm) is a new mineral, approved in 2024 and to date (February 2025) reported only from the type
locality.
Localities
At the type locality, the Jordanów serpentinite quarry, Gmina Jordanów Śląski, Wrocław County, Lower Silesian
Voivodeship, Poland, allanite-(Sm), the third samarium mineral to
be discovered, was found in a granitic
pegmatite in the
serpentinite quarry. It occurs as subhedral to anhedral crystals
with sizes of up to ~150 μm accompanied by allanite-(Nd),
allanite-(Y),
clinozoisite,
hingganite-(Y) and
xenotime-(Y). Allanite-(Sm) is yellowish brown with a white
streak and a vitreous lustre. It is brittle, with conchoidal fracture and imperfect cleavage.
Allanite-(Sm) and the associated allanite-(Y),
allanite-(Nd) and
hingganite-(Y) are
secondary minerals precipitated from calcium-rich
hydrothermal fluid during the metasomatic alteration of the
pegmatite. They accumulated
rare earth elements released by the alteration of nearby
xenotime-(Y)
(AM Research Article| September 20, 2024).
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