(For further information on spectroscopy, see:
http://speclab.cr.usgs.gov)
TITLE: Muscovite+Chlorite CU91-253D DESCRIPT
DOCUMENTATION_FORMAT: MIXTURE
SAMPLE_ID: CU91-253D
MIXTURE_TYPE: Intimate
MIXTURE: Chlorite and Muscovite in a Phyllite
FORMULA: (Mg,Fe)3(Si,Al)4O10(OH)2-(Mg,Fe)3(OH)6 and (Fe3+,Mg,Al,Fe2+,Ti,Mn)2.42(SiAl)2O5(OH)4
FORMULA_HTML: (Mg,Fe)3(Si,Al)4O10(OH)2-(Mg,Fe)3(OH)6
and (Fe3+Mg,Al,Fe2+,Ti,Mn)2.42(SiAl)2O5(OH)4
COLLECTION_LOCALITY: Cuprite, Nevada, USA
ORIGINAL_DONOR: Gregg Swayze
COLLECTION_LATITUDE: Not Available # degrees and decimal minutes (N or S)
COLLECTION_LONGITUDE: Not Available # degrees and decimal minutes (W or E)
DATUM: Not Available # coordinate datum
CURRENT_SAMPLE_LOCATION: U.S.G.S. Denver Spectroscopy Laboratory
ULTIMATE_SAMPLE_LOCATION: U.S.G.S. Denver Spectroscopy Laboratory
SAMPLE_DESCRIPTION:
Sample is a Chlorite - Muscovite phyllite from the Lower Cambrian Harkless Formation collected west of hwy 95 from south of the western relict hydrothermal center. This sample is from outside of the alteration zone and is representative of the regionally metamorphosed Harkless Formation.
END_SAMPLE_DESCRIPTION.
XRD_ANALYSIS:
none
END_XRD_ANALYSIS.
COMPOSITIONAL_ANALYSIS_TYPE: NONE # XRF. E,(WDS), ICP(Trace),WChem
COMPOSITION_TRACE: None
COMPOSITION_DISCUSSION:
none
END_COMPOSITION_DISCUSSION.
MICROSCOPIC_EXAMINATION:
none
END_MICROSCOPIC_EXAMINATION.
SPECTROSCOPIC_DISCUSSION:
Spectrum is dominated by Fe-related Chlorite absorptions in the electronic portion of the spectrum (.2 - 1.35 microns) and dominated by both muscovite and chlorite absorptions in the vibrational region (1.35 - 2.5 microns). There is a Al-OH combination band from Al-rich muscovite at 2.1970 microns. Bands at 2.2596 and 2.3461 microns are due to chlorite.
END_SPECTROSCOPIC_DISCUSSION.
SPECTRAL_PURITY: 1a2_3_4_ # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns
LIB_SPECTRA_HED: | where | Wave Range | Av_Rs_Pwr | Comment |
---|---|---|---|---|
LIB_SPECTRA: | splib05a r 8723 | 1.3-5.3µm | 200 | g.s.= |
LIB_SPECTRA: | splib06a r 26061 | g.s.= |