The garnets constitute a group of minerals which share a common structure. Common end member compositions are:
As would be expected from a chemically complex group of minerals, garnets owe their color to a variety of causes. Absorption by Cr3+, V3+, Fe3+ (6-coordinated site), Fe2+ (8-coordinated site), Mn2+, and Fe2+ - Ti4+ intervalence charge transfer can all be found in the spectra of garnets.
Almandine GRR 892, India. 1.0 mm thick
Almandine GRR 1040, North River Garnet Company, Warren Co., NY, [Fe1.35 Mg1.30 Ca0.26 Mn0.03] Al1.98(SiO4)3; 1.54 mm thick; data file Almandine, GRR 1056, Wrangell, Alaska, [Fe2.03Mg0.67Ca0.18Mn0.07]Al2.0(SiO4)3, colored light reddish-purple by Fe2+ , normalized to 1.0 mm thickness; data file
Almandine, GRR 1776, dark reddish-purple gemstone, [Fe2.5Mg0.3Mn0.2Ca0.1]Al2.0(SiO4)3, probably from India, Graphed at 1.0 mm, normalized from 0.213 mm thickness. Visible region only; data file Pyrope, GRR 83, rhodolite variety, Umba River Valley, Tanzania, colored pink by Fe2+; 0.78 mm thick; data file Pyrope, GRR 131, unknown locality, probably Tanzania, colored pink by Fe2+ ; Approximate 8-coordinated site composition: Mg1.82 Fe0.99 Ca0.04 Mn0.04. Plotted as 2.007 mm thick; data file
Pyrope, GRR 1121i, Wesselton, South Africa, Mg2.32 Mn0.01 Fe0.43 Ca0.27 Al1.95 Cr0.02, 1.693 mm thick; data file Pyrope, GRR 1121f, Wesselton kimberlite diamond mine, South Africa. Mg2.09 Mn0.02 Fe0.67 Ca0.26 Al1.89 Cr0.03 Ti0.03. Plotted as 0.547 mm thick; data file; data file Pyrope-spessartine, GRR 1267, Kenya, sold commercially as "Malaya Garnets". 1.686 mm thick; data file Pyrope, Mon-9, Monastery Mine, South Africa, 1.37 mm thick; data file . Showing the three near-IR Fe2+ bands in the 1000 - 2500 nm range and weaker broad OH bands that are visible in the 2800 nm region.
,
expanded view from a
2.165 mm thick sample. data file
due to the mixture of Fe, Mn and Ti. Approximate compositon: Ca2.23,
Mn0.72, Fe1.48, Al0.44, Ti0.02. Plotted as 1.0 mm thick.
,
San Benito Mountains, California, with both Fe3+
and Ti4+, 0.102 mm thick. Approximate composition in the 6-coordinated site: Fe1.16, Ti0.74, Al0.007. data
file
are
black, but when
thinned, it becomes dark brown-orange. The sharp peak near 441
nm is
from Fe3+; approximate composition in the 6-coordinated site: Fe1.69, Ti0.27, Al0.04. 0.045 mm thick, data file
. Jeffrey Mine, Asbestos (now Val-des-Sources), Québec, Canada
,
2.084 mm thick. Data file.
, 4.126 mm thick. Data file
,
colored
greenish-yellow by Fe3+, nesr end-member comopsition. Plotted as 1.03 mm
thick; data
file.
,
colored by Fe3+, 0.737 mm thick; data
file.
These garnets vary from green to brownish. Data files: green;
brown
plotted as 1.00 mm thick. This light green garnet
has the spectrum with the least deviation from pure andradite. Data file
. Approximate composition of the 6-coordiated site: Cr1.19 Fe0.57 Al0.15 Ti0.04 V0.01. Plotted as
0.029 mm thick. data file
,
colored green by 0.11 wt% V3+. Plotted as 0.758 mm thick. data
file
,
2.5 mm thick.The spectrum of the slab
has both the features of Fe3+ and the features
of Cr3+. Data
file.
and
green after
heat-treatment
which
is used to remove the brown component of color
often found in the
natural stones. Data files: GRR 2666 - orange;
GRR 2667 - green
,
Chromian-pyrope, Ca0.33 Mn0.02
Mg2.13 Fe0.54 Al1.95
Cr0.07, 0.840 mm thick; data file
.
They contain about 1 to 1.5% manganese oxide. Only about 10 percent of
the manganese, which is in the 3+ oxidation state, is
responsible
for the pink color. Data
File.
that
goes from pale purplish-blue to light purple depending upon
the
illumination. It contains about 0.6 wt% vanadium. Thickness: 2.426 mm. Data
file.
from the
Merelani Hills, Tanzania . Data files; RT,
LN2
from Asbestos, Ontario,
Canada. Data file: RT
, from the Lelatema Mountains, Tanzania. Data files: RT, -78 C
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