- Modality
- FTIR
- Category
- mineral
- Material Type
- Nesosilicate
- Sample ID
- HS113.3B-HCL
- Collection Locality
- Transvaal, S. Africa
- Spectral Purity
- 1d2c3c4c # 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 Andradite, with Hydrogrossular, with Uvarovite. In this sample some ferrous ion has substituted for calcium, producing the 1.0 µm absorption and some ferric ion has substituted for aluminum, producing the band near 0.8 µm. Such substitution is common for this mineral. The presence of Fe accounts for the absorption features near 0.6 and 0.43 µm and the series of bands between 1.4 and 1.51 µm are due to OH substitution for SiO4. Carbonate impurities cause absorption features near 2.25, 2.35, and 2.5 µm. 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: .3B = 74-250 µm See additional spectra of grossular garnets in library for comparison. This sample has been washed in HCl acid to remove carbonate contaminants. IMAGE_OF_SAMPLE:
- XRD Analysis
- Grossular + feldspar + others (Norma Vergo, USGS)
- X Units
- cm⁻¹
- Y Units
- Absorbance
- Data Points
- 1,801