Clinochlore

Clinochlore — NIR2,126 points · 400012500 cm⁻¹
400060008000100001200000.05000.1000.150Wavenumber (cm⁻¹)Absorbance
Clinochlore sample photograph, USGS Spectral Library Version 7
Sample photograph — USGS Spectral Library v7

Spectrum Details

Modality
NIR
Category
mineral
Material Type
Phyllosilicate
Sample ID
GDS158
Collection Locality
Flagstaff Hill, California ORIGINAL_DONOR: Jim Post CURRENT_SAMPLE_LOCATION: USGS Denver Spectroscopy Laboratory ULTIMATE_SAMPLE_LOCATION: USGS Denver Spectroscopy Laboratory SAMPLE_DESCRIPTION:
Spectral Purity
1b2b3b4_ # 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
This sample described in: Post, J.L. and C.C. Plummer, 1972, The chlorite series of Flagstaff Hill area, California: A preliminary investigation. Clays and Clay Minerals, v.20, pp271-283. Clinochlore was previously called Sheridanite. IMAGE_OF_SAMPLE:
XRD Analysis
45 kV - 35 mA, 6.5-9.5 keV, smear mount (sherd8.out); 40 kV - 30 mA, random mount (sherd8-2.out) References: Bailey (1988, MSA Reviews 19; 1988 in Clays and Clay Minerals); Huebner's reference patterns Found: Chlorite type IIbb. A broad, very weak reflection at 9.6 is probably due to a trace of mica. A weak reflection at 3.23 Angstroms may be due to a trace of feldspar. A weak unidentified reflection at 2.357 Angstroms. And a weak, unidentified reflection at 7.8 Angstroms that also appeared in GDS157 (the "ripidolite"). Sought but not found: quartz Comments: With chemical analysis, the chlorite is a clinochlore IIbb. Severe preferred orientation in smear mounts; fortunately, there was enough sample for a random mount. Sharp chlorite reflections indicate excellent crystallinity. With GDS157 ("ripidolite"), the best chlorite patterns I have ever seen." J.S. Huebner, J. Pickrell, and T.Schaefer, 1994, written communication. 40 kV- 30 mA, 7.3-9.5 keV File sherd158.out, -.mdi (edge/random mount) References: Bailey (1988 in Clays and Clay Minerals, 36, 193-213); Huebner's reference patterns Found: clinochlore type IIbb, trace rutile Comment: Sharp reflections suggest excellent crystallinity and compositional homogeneity. Position of the (060) reflection indicates Mg/(Mg+Fe+Mn) = 0.85. Presence of rutile confirmed optically; rutile forms thin but very elongate needles in the chlorite flakes ("rutilated clinochlore").
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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