(For further information on spectroscopy, see:
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TITLE: Dickite + others CU91-219B DESCRIPT
DOCUMENTATION_FORMAT: MIXTURE
SAMPLE_ID: CU91-219B
MIXTURE_TYPE: Intimate
MIXTURE: Dickite, Kaolinite, Quartz, Calcite
FORMULA: Al2Si2O5(OH)4, Al2Si2O5(OH)4, SiO2, CaCO3
FORMULA_HTML: Al2Si2O5(OH)4 Al2Si2O5(OH)4 SiO2, CaCO3
COLLECTION_LOCALITY: Eastern Alteration Center, Cuprite, Nevada, USA
ORIGINAL_DONOR: Gregg Swayze
COLLECTION_LATITUDE: N37 31.90' # degrees and decimal minutes (N or S)
COLLECTION_LONGITUDE: W117 13.30' # degrees and decimal minutes (W or E) P> DATUM: NAD27 # coordinate datum
CURRENT_SAMPLE_LOCATION: U.S.G.S. Denver Spectroscopy Laboratory
ULTIMATE_SAMPLE_LOCATION: U.S.G.S. Denver Spectroscopy Laboratory
SAMPLE_DESCRIPTION:
This sample was collected from the southwestern portion of the western alteration center at Cuprite, NV and is composed of hydrothermally altered lower Cambrian Harkless Phyllite altered during a 7.5 Ma hydrothermal event.
END_SAMPLE_DESCRIPTION.
XRD_ANALYSIS:
Dickite plus some solid solution with kaolinite, quartz, and calcite.
END_XRD_ANALYSIS.
COMPOSITIONAL_ANALYSIS_TYPE: XRF # XRF, EM(WDS), ICP(Trace), WChem
COMPOSITION_TRACE: None
COMPOSITION_DISCUSSION:
None
END_COMPOSITION_DISCUSSION.
MICROSCOPIC_EXAMINATION:
None
END_MICROSCOPIC_EXAMINATION.
SPECTROSCOPIC_DISCUSSION:
The spectrum doesn't include the spectral range from 0.35-1.35 microns. The spectral absorptions are characteristic of dickite with strong doublets in the 1.4 and 2.2 micron region.
See: Swayze, G.A., 1997, The hydrothermal and structural history of the Cuprite Mining District, southwestern Nevada: an integrated geological and geophysical approach: unpublished Ph.D. Dissertation, University of Colorado at Boulder, 399p.
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 8030 | 1.3-5.3µm | 200 | g.s.= |
LIB_SPECTRA: | splib06a r 24979 | g.s.= |