Pyrite — NIR2,126 points · 400012500 cm⁻¹
400060008000100001200000.02000.04000.06000.0800Wavenumber (cm⁻¹)Absorbance

Spectrum Details

Modality
NIR
Category
mineral
Material Type
Sulfide
Sample ID
GDS483.c
Collection Locality
Armejun, Spain
Spectral Purity
1c2c3d4b # GDS483.c # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns
Composition / XRD
None # XRF, EPMA, ICP(Trace), WChem
Sample Description
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

License: Public Domain

DOI: 10.3133/ds1035

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