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- W2016520370 abstract "Abstract Benleonardite, ideally Ag 8 (Sb,As)Te 2 S 3 with Sb > As, is a new mineral species that occurs in ore specimens collected from the dumps of the disused Bambolla mine, Moctezuma, Mexico. The associated minerals are acanthite, hessite, an unnamed Ag 4 TeS phase, pyrite, sphalerite, and native silver. Together with benleonardite, these form thin black crusts in fractures filled with quartz and dolomite in highly altered, tuffaceous, andesitic and rhyolitic rocks. Benleonardite is an opaque mineral and, in reflected plane-polarized light in air, it is weakly bireflectant from very pale light blue to slightly darker blue. It is not pleochroic. Luminance values (relative to the CIE illuminant C ) for R o and R ′ e computed from visible spectrum reflectance data for the most bireflectant grain, are 33.6 and 31.7% in air, and 18.3 and 16.5% in Zeiss oil ( N D 1.515) respectively. Vickers micro-indentation hardness is 105–125 (VHN 25 ). The X-ray powder diffraction pattern could be indexed on a tetragonal cell with a 6.603(5) and c 12.726(6) Å; for Z = 2, the calculated density is 7.79 g/cm 2 for the average analysis. The strongest five lines in the X-ray powder pattern are [ d in Å ( I ) ( hkl ): 12.7 (70) (001); 3.188 (30) (021,004); 2.936 (100) (022); 2.608 (35) (023); 2.158 (35) (124)." @default.
- W2016520370 created "2016-06-24" @default.
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- W2016520370 date "1986-12-01" @default.
- W2016520370 modified "2023-09-26" @default.
- W2016520370 title "Benleonardite, a new mineral from the Bambolla mine, Moctezuma, Sonora, Mexico" @default.
- W2016520370 cites W2002488775 @default.
- W2016520370 doi "https://doi.org/10.1180/minmag.1986.050.358.15" @default.
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