PPL: color in brown and yellow tones with pink, similar to bornite. It tarnishes very quickly to brown. Weak to absent pleochroism. Reflectivity from 37 to 42%, no bireflectance.
XPL: strong anisotropy from yellow-gray to soft green, gray to bluish. Brown color is strong, blue is more discreet. No internal reflections.
Images: Arsenopyrite (PPL = white) and pyrrhotite in PPL and XPL. The gray-brown colors of pyrrhotite are very easy to identify.
PPL: gray-brown to gray-rose color, without pleochroism. Reflectivity of 19%, with weak bireflectance (see grain limits and twins!). It is a very common opaque in many igneous and metamorphic rocks, along with magnetite.
XPL: strong anisotropy in shades of gray, one of the colors has a well-defined bluish tone (observe with CPL+2º). Very rare reflections.
Images: Ilmenite in PPL (gray-rose) and in XPL (gray-bluish).
PPL: copper red to light grayish orange color, very similar to bornite color. No pleochroism. 31.5% reflectivity, no bireflectance. It always occurs as a fine lamellar alteration product in bornite. It does not tarnishes, unlike bornite.
XPL: very strong anisotropy between blue-green (turquoise) and reddish brown. No internal reflections.