“Reflected light digital image, partly crossed polarizers (1 mm wide) of a colloform aggregate of native arsenic (bright) The interstitial minerals are proustite (crimson red internal reflectance), argentopyrite (light-brown, cream), chalcopyrite (yellow) and sphalerite (grey)..
Reference:
Grundmann, G. (1971): Neues über Silbererze vom Tannenbodengang bei Wieden (Südschwarzwald). Der Aufschluss Volume 22, No. 6/1971, p. 195-200.
G. Grundmann collection and photo.
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Dr. Günter Grundmann - 27th March 2018