DOCUMENTATION_FORMAT: MINERAL
SAMPLE_ID: ISR202
MINERAL_TYPE: Phyllosilicate
MINERAL: Rectorite
FORMULA: Al2Si4O10(OH)2 + (Mg,Fe+2,Al)3(Al,Si)4O10(OH)2*4H2O
FORMULA_HTML: Al2Si4O10(OH)2 + (Mg,Fe+2,Al)3(Al,Si)4O10(OH)2•4H2O
COLLECTION_LOCALITY: Garland County, Arizona
ORIGINAL_DONOR: Not available
CURRENT_SAMPLE_LOCATION: CSES/CIRES, Univ. of CO, Boulder
ULTIMATE_SAMPLE_LOCATION: CSES/CIRES, Univ. of CO, Boulder
SAMPLE_DESCRIPTION:
Rectorite, a clay mineral, is a regular interstratification of a dioctahedral mica and a dioctahedral smectite.
IMAGE_OF_SAMPLE:
NO PHOTO
END_SAMPLE_DESCRIPTION.
XRD_ANALYSIS:
Not Available
END_XRD_ANALYSIS.
COMPOSITIONAL_ANALYSIS_TYPE: None # XRF, EPMA, ICP(Trace), WChem
COMPOSITION_TRACE:
COMPOSITION_DISCUSSION:
END_COMPOSITION_DISCUSSION.
MICROSCOPIC_EXAMINATION:
mode:
Rectorite dominates
20 vol% quartz
muscovite & chlorite undetermined
quartz average grain size= 300 µm
all others average grain size= 35 µm
Rectorite forms fine intergrowths with muscovite & chlorite
END_MICROSCOPIC_EXAMINATION.
SPECTROSCOPIC_DISCUSSION:
END_SPECTROSCOPIC_DISCUSSION.
SPECTRAL_PURITY: 1d2_3_4_ # ISR202 # 1= 0.2-3, 2= 1.5-6, 3= 6-25, 4= 20-150 microns