In:
Mineralogical Magazine, Mineralogical Society, Vol. 50, No. 356 ( 1986-06), p. 279-282
Abstract:
Laphamite, ideally As 2 (Se,S) 3 , is monoclinic, P2 1 /n , with a = 11.86(1), b = 9.756(9), c = 4.265(9) Å, β = 90.17°, V = 493.5 Å 3 , Z = 4, D (calc.) = 4.60, D (meas.) = 4.5(1) g/cm 3 . Microprobe analysis yielded: As 47.0, Se 43.7, S 8.7, sum = 99.4 wt. %. In plane polarized light in polished section at about 3200 K laphamite is moderately bireflectant from white to grey. Reflection pleochroism is absent but fiery red internal reflections are characteristic as are golden yellow reflections along scratches. Anisotropy is moderate with grey rotation tints, masked in some sections by internal reflections. Reflectance spectra in air and oil between 400 and 700 nm are given. Colour values for the CIE illiminant C in air are, for R 1 followed by R 2 : Y % 29.0, 33.5, λ d 480, 478; P e % 9.1, 8.7. Laphamite forms dark red crystals, up to 5.0 mm, associated with orpiment, arsenolite, and an unnamed phase, NH 4 AlF 4 , in a burning coal waste-dump at Burnside, Northumberland County, Pennsylvania.
Type of Medium:
Online Resource
ISSN:
0026-461X
,
1471-8022
DOI:
10.1180/minmag.1986.050.356.11
Language:
English
Publisher:
Mineralogical Society
Publication Date:
1986
detail.hit.zdb_id:
2034522-7
SSG:
13
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