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(For further information on spectrsocopy, see:
http://speclab.cr.usgs.gov)
TITLE: Limestone CU02-11A DESCRIPT
DOCUMENTATION_FORMAT: MIXTURE
SAMPLE_ID: CU02-11A
MIXTURE_TYPE: Intimate
MIXTURE: Limestone
FORMULA: CaCO3 + impurities
FORMULA_HTML: CaCO3 + impurities
COLLECTION_LOCALITY: 6 km north of western center, Cuprite, Nevada, USA
ORIGINAL_DONOR: Gregg Swayze
COLLECTION_LATITUDE: N37 36.908' # degrees and decimal minutes (N or S)
COLLECTION_LONGITUDE: W117 14.393' # 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 a large outcrop of the Cambrian Mule Springs Limestone exposed about 6 km north of the western alteration center at Cuprite, NV. The surface measured spectrally is the weathered surface of the sample.
END_SAMPLE_DESCRIPTION.
XRD_ANALYSIS:
calcite (major), quartz (trace)
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 has absorptions that are characteristic of calcite with a main C-O related absorption at 2.3391 microns. The monotonic negative slope toward shorter wavelengths may be caused by oranic impurities.
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history of the Cuprite Mining District, southwestern Nevada: an integrated geological and geophysical approach: unpublished Ph.D. Dissertation, University of Colorado at Boulder, 399p.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 8575 | 0.2-3.0µm | 200 | g.s.= |
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