Staurolite

Staurolite — NIR2,126 points · 400012500 cm⁻¹
400060008000100001200000.02000.04000.06000.0800Wavenumber (cm⁻¹)Absorbance
Staurolite sample photograph, USGS Spectral Library Version 7
Sample photograph — USGS Spectral Library v7

Spectrum Details

Modality
NIR
Category
mineral
Material Type
Nesosilicate
Sample ID
HS188.1B, HS188.2B, HS188.3B, HS188.4B
Collection Locality
Fannin County, Georgia
Spectral Purity
1b2_3_4_ # HS188.1B # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns SPECTRAL_PURITY: 1b2_3_4_ # HS188.2B # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns SPECTRAL_PURITY: 1c2c3d4_ # HS188.3B # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns SPECTRAL_PURITY: 1c2_3_4_ # HS188.4B # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns
Composition / XRD
None # XRF, EPMA, ICP(Trace), WChem COMPOSITION_TRACE:
Sample Description
N-14 Staurolite 188B--Fannin Co., Georgia. (Fe^2+, Mg)2(Al, Fe^3+)9O6 (SiO4)4(O, OH)2: Staurolite, like kyanite and sillimanite is a typical mineral found in medium grade metamorphosed argillaceous rocks. It is produced at a lower temperature-pressure than is kyanite. This spectrum shows strong general absorption to both long and short wavelengths which produces an apparent reflectivity maximum near 1.05 µ. The fall off to longer wavelengths must be due to generalized hydroxyl and water absorptions and is quite similar in appearance to the spectrum of diaspore (see Part III, p. 200, spectrum (-6). The fall off in the visible must be due to absorptions by ferrous and ferric iron. Hunt, G.R., J.W. Salisbury, and C.J. Lenhoff, 1973, Visible and near-infrared spectra of minerals and rocks: VI. Additional silicates. Modern Geology, v. 4, p. 85-106. 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: staur188.out, -.mdi References: JCPDS # 41-1484; Huebner's reference patterns Found: quartz, staurolite, K-mica Comment: All components appear well crystallized and in significant representation with quartz, staurolite, mica. All reflections are accounted for. The mica basal reflection at 10 Angstroms appears to be a doublet but next 4.95 does not. J.S.Huebner, J. Pickrell, T. Schaefer, written communication(1994 USGS)
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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