- Modality
- FTIR
- Category
- mineral
- Material Type
- Nesosilicate
- Sample ID
- GDS12
- Collection Locality
- Esmerald Co., Nevada
- Spectral Purity
- 1c2c3c4_ # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns
- Composition / XRD
- EPMA # XRF, EPMA, ICP(Trace), WChem
- Sample Description
- Forms series with Grossular and with Schorlomite. Sample is ground and sieved to less than 250 µm. Compare with other Andradite samples in library because spectral differences do exist between samples. Spectral features near 2.3 µm indicate trace spectral contamination. From the analyses below and the band position and shape, this appears to be calcite. Roger N. Clark IMAGE_OF_SAMPLE:
- XRD Analysis
- 40 kV - 30 mA, 7.3-9.5 keV File: angds12.out, *.mdi References: Huebner's reference patterns Found: Garnet, probable clinopyroxene and alkali feldspar (two?) Comment: Difficult pattern to decipher. Four garnet compositions are resolved; the dominant garnet has ao=11.87 Angstroms, consistent with grossular-rich garnet. Other garnet compositions have larger cell dimensions (to ao=11.98 Angstroms), indicating andradite or uvarovite component. Based on brown color, the minor garnet compositions are andradite-rich. Many weak to very weak reflections are best described as a clinopyroxene (augite, not hedenbergite) and alkali feldspar (microcline + low albite). Optics are consistent; isotropic garnet, a low-birefringence phase with about 1.53 refractive index, and a moderate birefringence phase with about 1.69 refractive index.
- X Units
- cm⁻¹
- Y Units
- Absorbance
- Data Points
- 1,801