Forms series with Cattierite (CoS2). Dimorphous with Marcasite. "SS-19. Pyrite. Rico, Colorado (35). Pyrite, FeS2, is the most common and widespread of sulphides. It occurs in igneous, metamorphic and sedimentary rocks, as well as in veins. In the visible, pyrite displays the reflectivity vs. particle size behavior that is peculiar to opaque minerals - ie. reflectivity decreases as particle size decreases. It is also interesting that decreased absorption in the red region of the visible results in a significant contrast in reflectivity from the red to the blue, despite the sample's overall low reflectivity. In the near-infrared, the spectral behavior of pyrite changes from that of an opaque material to that of a transparent one. This sample was ground from one of the original cubes of pyrite. Grain size fractions are indicated by the extension after the sample number: .a = 1000µm IMAGE_OF_SAMPLE: Not Available
XRD Analysis
Major pyrite with minor szomolnokite and minor rhomboclase. (Steve Sutley)
X Units
cm⁻¹
Y Units
Absorbance
Data Points
2,126
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Attribution
USGS Spectral Library Version 7, U.S. Geological Survey