(For further information on spectrsocopy, see:
http://speclab.cr.usgs.gov)
TITLE: Kaolin_Smect H89-FR-2 .5Kaol DESCRIPT
DOCUMENTATION_FORMAT: MIXTURE
SAMPLE_ID: H89-FR-2
MIXTURE_TYPE: Intimate
MIXTURE: Kaolinite/Smectite (50% Kaol.)(Kaolinite-Serpentine group)
FORMULA: Al2Si2O5(OH)4 + (Na,Ca)0.33(Al,Mg)2Si4O10(OH)2*nH2O
FORMULA_HTML: Al2Si2O5(OH)4 + (Na,Ca)0.33(Al,Mg)2Si4O10(OH)2•nH2O
COLLECTION_LOCALITY: Paris Basin, France
ORIGINAL_DONOR: Phoebe Hauff, Fred Kruse CSES/CIRES
CURRENT_SAMPLE_LOCATION: CSES/CIRES, Univ. of CO, Boulder
ULTIMATE_SAMPLE_LOCATION: CSES/CIRES, Univ. of CO, Boulder
SAMPLE_DESCRIPTION:
Kaolinite/smectite clays are produced as transitional phases as smectite weathers to kaolinite. This sample is from the Argiles Plastique Formation of the Paris Basin. This formation contains a paragentic sequence from smectite to kaolinite.
Hauff, P.L., F.A. Kruse, and Medard Thiry, 1990, Spectral identification and characterization of kaolinite/smectite clays in weathering environments. Proceedings of the Fifth Australian Remote Sensing Conference, Perth, Australia, pp. 898-905.
END_SAMPLE_DESCRIPTION.
XRD_ANALYSIS:
XRD was used to determine the percent kaolinite. In this case, the sample is 50% kaolinite.
Hauff, P.L., F.A. Kruse, and Medard Thiry, 1990, Spectral identification and characterization of kaolinite/smectite clays in weathering environments. Proceedings of the Fifth Australian Remote Sensing Conference, Perth, Australia, pp. 898-905.
END_XRD_ANALYSIS.
COMPOSITIONAL_ANALYSIS_TYPE: None # XRF, EM(WDS), ICP(Trace), WChem
COMPOSITION_TRACE: None
COMPOSITION_DISCUSSION:
END_COMPOSITION_DISCUSSION.
MICROSCOPIC_EXAMINATION:
END_MICROSCOPIC_EXAMINATION.
SPECTROSCOPIC_DISCUSSION:
END_SPECTROSCOPIC_DISCUSSION.
SPECTRAL_PURITY: 1b2_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: | splib04a r 2643 | 0.2-3.0µm | 200 | g.s.= |
LIB_SPECTRA: | splib05a r 8513 | 0.2-3.0µm | 200 | g.s.= |
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