Chalcopyrite

Chalcopyrite — FTIR1,801 points · 4004000 cm⁻¹
500100015002000250030003500400000.02000.04000.06000.0800Wavenumber (cm⁻¹)Absorbance
Chalcopyrite sample photograph, USGS Spectral Library Version 7
Sample photograph — USGS Spectral Library v7

Spectrum Details

Modality
FTIR
Category
mineral
Material Type
Sulfide
Sample ID
HS431.1B, HS431.2B, HS431.3B, HS431.4B
Collection Locality
Quebec
Spectral Purity
1b2_3_4_ # Chalcopyrite HS431.1B # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns SPECTRAL_PURITY: 1b2_3_4_ # Chalcopyrite HS431.2B # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns SPECTRAL_PURITY: 1b2b3c4_ # Chalcopyrite HS431.3B # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns SPECTRAL_PURITY: 1b2_3_4_ # Chalcopyrite HS431.4B # 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 Eskebornite. Spectra for this sample were originally published in: Hunt, G.R., J.W. Salisbury, and C.J. Lenhoff, 1971, Visible and near-infrared spectra of minerals and rocks: IV. Sulfides and sulfates Modern Geology, v. 3, p. 1-14. With the note: "It exhibits typical opaque behavior, decreasing in reflectivity as its particle size is reduced. It is not, however, spectrally featureless. A fall-off in the reflectivity toward the blue, together with a weak band near 0.9µm, results in the characteristic brass-yellow color of this mineral. Both spectral features are due to iron, which is present in chalcopyrite in the trivalent state (Deer and others, 1962). The copper also makes a contribution to the feature near 0.9µm. This sample is contaminated with approximately 10% pyrrhotite, which has no appreciable effect on the spectrum." Grain size fractions are indicated by the extension after the sample number: .1B = IMAGE_OF_SAMPLE:
XRD Analysis
40 kV - 30 mA, 7.3-9.5 keV File: chpyr431_mdi, *.out (smear mount on quartz plate) References: JCPDS #37-471, #5-566; Huebner's reference patterns Found: Chalcopyrite, minor sphalerite Comment: Moderately sharp, symmetrical peaks suggest moderate crystallinity and compositional heterogeneity. Sphalerite lattice spacing's consistent with ZnS composition (Fe-poor sphalerite). J.S. Huebner, J. Pickrell, and T. Schaefer, 1994, written communication.
X Units
cm⁻¹
Y Units
Absorbance
Data Points
1,801

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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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