- Modality
- FTIR
- Category
- mineral
- Material Type
- Carbonate
- Sample ID
- HS102.1B, HS102.3B, HS102.4B
- Collection Locality
- Lee, MA
- Spectral Purity
- 1b2_3_4_ # Dolomite HS102.1B # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns SPECTRAL_PURITY: 1b2b3b4b # Dolomite HS102.3B # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns SPECTRAL_PURITY: 1b2_3_4_ # Dolomite HS102.4B # 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
- .p> Forms series with Ankerite and with Kutnohorite. "This is a recrystallized dolomitic marble, which displays the carbonate absorption features at longer wavelengths than typical for calcites. Weak absorption band at 1.0µm is due to ferrous iron, which is shown to be present at 0.03 wt.% in the sample." Hunt, G.R., J.W. Salisbury, 1971, Visible and near-infrared spectra of minerals and rocks: II. Carbonates. Modern Geology, v. 2, p. 23-30. Grain size fractions are indicated by the extension after the sample number: .1B = IMAGE_OF_SAMPLE:
- XRD Analysis
- Dolomite plus trace of calcite XRD done by Norma Vergo Clark, R.N., King, T.V.V., Klejwa, M., Swayze, G.A., and Vergo, N., 1990, High spectral resolution reflectance spectroscopy of minerals: Journal of Geophysical Research, v. 95, no. 8B, p 12,653-12,680.
- X Units
- cm⁻¹
- Y Units
- Absorbance
- Data Points
- 1,801