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Kyanite, Sillimanite, and Andalusite Deposits of the Southeastern ...

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GEOLOGY OF THE DEPOSITS 9<br />

TABLE 3. Chemical <strong>and</strong> spectrochemical analyses <strong>of</strong> kyanite<br />

quartzite <strong>and</strong> sillimanite quartzite from Farmville district,<br />

Virginia, <strong>and</strong> Kings Mountain district, North Carolina-<br />

South Carolina<br />

VB-W<br />

Ky anite quartzite<br />

SY-87<br />

NG-437<br />

<strong>Sillimanite</strong> quartzite<br />

NG-439<br />

NG-440<br />

Chemical analyses<br />

[VB-W: L. D. Trumbull, analyst; SY-87, NG-437, NG-439, NG-440: L. N.<br />

Tarrant, analyst]<br />

Location <strong>of</strong> samples:<br />

VB-W, Lab. No. 53-835SCD. Composite sample <strong>of</strong> kyanite quartzite<br />

from 6 pieces <strong>of</strong> diamond-drill core from 5 drill holes, Willis Mountain,<br />

Buckingham County, Va.<br />

SY-87, Lab. No. 52-1611CDSW. Composite sample <strong>of</strong> kyanite quartzite<br />

taken from 6 places in nor<strong>the</strong>rn opencut <strong>of</strong> Commercialores, Inc.,<br />

Henry Knob, York County, S.C.<br />

NG-437, Lab. No. 52-1605CDSW. Composite sample <strong>of</strong> 6 pieces <strong>of</strong><br />

kyanite-chloritoid quartzite taken across strike <strong>of</strong> 10-foot bed, 1.2 miles<br />

S. 10° W. <strong>of</strong> Crowders Mountain Village, Gaston County, N.C.<br />

NG-439, Lab. No. 52-1607CDSW. Composite sample <strong>of</strong> 6 pieces <strong>of</strong> sillimanite<br />

quartzite from crest <strong>of</strong> Reese Mountain, Lincoln County, N.C.<br />

NG-440, Lab. No. 52-1608CDSW. Composite sample <strong>of</strong> 6 pieces <strong>of</strong> sillimanite<br />

quartzite from Will Knox property, Gaston County, N.C.<br />

SiO 2 ...............<br />

Fe 2O3.. ............<br />

FeO<br />

MgO...............<br />

CaO...............<br />

Na2O ..............<br />

K2O ...............<br />

H2O ..............<br />

H2O + .............<br />

TiC-2...............<br />

CO2 . ..............<br />

P 2Os.........<br />

F..... .............<br />

S.. ................<br />

MnO. .............<br />

68.71<br />

27.61<br />

.57<br />

.04<br />

.14<br />

.41<br />

.00<br />

.14<br />

.04<br />

.32<br />

1.02<br />

.02<br />

.32<br />

.00<br />

73.56<br />

17.01<br />

.00<br />

5.25<br />

.01<br />

.00<br />

.00<br />

.00<br />

.01<br />

.12<br />

.48<br />

.01<br />

4.62<br />

.00<br />

63.35<br />

28.97<br />

2.25<br />

2.50<br />

.31<br />

.07<br />

.13<br />

.04<br />

.05<br />

1.30<br />

.86<br />

.01<br />

09<br />

.05<br />

75.33<br />

23.36<br />

.04<br />

.18<br />

.01<br />

.01<br />

.02<br />

.10<br />

.02<br />

.19<br />

.60<br />

.02<br />

.06<br />

.00 (Tr.)<br />

69.59<br />

27.24<br />

.17<br />

.13<br />

.01<br />

.17<br />

.00<br />

.00<br />

.01<br />

.58<br />

1.46<br />

.02<br />

.33<br />

.03<br />

.00 (Tr.)<br />

Total... ..........<br />

Less O for F. .....<br />

Less O for S ......<br />

99.55<br />

.09<br />

101.18<br />

1.16<br />

99.74<br />

.01<br />

Total. ...........<br />

99.46<br />

100.02<br />

99.98<br />

99.94<br />

99.73<br />

Spectrochemical analyses<br />

[P. R. Barnett, analyst. Zeros in unit column signify that <strong>the</strong> elements<br />

were not detected; sensitivity limits for <strong>the</strong>se elements are: B, 0.003;<br />

Be, 0.0001; Co, 0.0005 ; Ga, 0.0005 ; La, 0.005 ; Mo, 0.0001; Ni, 0.0003 ; Pb,<br />

0.0006 ; Sn, 0.001; Sr, 0.0008 ; Y, 0.001 ; Yb, 0.0001; Zn, 0.01. Elements not<br />

detected in any <strong>of</strong> <strong>the</strong>se samples, toge<strong>the</strong>r with <strong>the</strong>ir sensitivity limits, are:<br />

Ag, 0.0005; As, 0.05; Au, 0.003; Bi, 0.001 ; Cd, 0.005; Ge, 0.0005; In,<br />

0.001; Nb, 0.001; Pt, 0.003 ; Sb, 0.01 ; Ta, 0.05 ; Th, 0.05 ; Tl, 0.01; U, 0.05 ;<br />

W, 0.01]<br />

B..... ...... .......<br />

Ba..... .......<br />

Be..... ............<br />

Co..... ....<br />

Cr. ................<br />

Cu ................<br />

Ga. . ............<br />

La.................<br />

Mo.... ........<br />

Ni... ......<br />

Pb.........<br />

So.......... .....<br />

Sn.........<br />

Sr .................<br />

V........ .. .. .<br />

Y.....<br />

Yb. ....... .....<br />

Zn.... .....<br />

Zr.........<br />

0 0<br />

.02<br />

.04<br />

0 0<br />

0 .001<br />

.002 .0004<br />

.001<br />

0<br />

.0005<br />

0 .008<br />

.002 .0007<br />

0 .0003<br />

.001 0<br />

.0001 .0004<br />

.002 0<br />

.4<br />

.09<br />

.1<br />

.009<br />

.002 .002<br />

0 .0003<br />

0<br />

.01<br />

.04<br />

0004<br />

0<br />

0<br />

.006<br />

.002<br />

0<br />

0<br />

.0003<br />

.001<br />

.002<br />

0<br />

.0008<br />

.06<br />

.002<br />

0<br />

.01<br />

.0002<br />

.03<br />

.01<br />

0<br />

.0006<br />

0<br />

0<br />

.003<br />

.08<br />

.0001<br />

0<br />

.01<br />

.0007<br />

.0006 .003<br />

0<br />

.01<br />

0<br />

.0004<br />

0<br />

.0003<br />

0 .0006<br />

.0001 .0009<br />

.003 0<br />

0 .5<br />

.006 .03<br />

0<br />

0<br />

0<br />

.02<br />

.002<br />

.0001<br />

0<br />

.02<br />

FIGURE 1. Photomicrograph <strong>of</strong> kyanite-quartz rock from Graves Mountain,<br />

Lincoln County, Ga. Shows kyanite (k), fine-grained quartz (q), relict<br />

phenocryst <strong>of</strong> blue (bq), a little muscovite( ?) (m), <strong>and</strong> rutile (r). Rock<br />

is highly wea<strong>the</strong>red <strong>and</strong> contains much limonite (1). Holes in section (h).<br />

Crossed nicols.<br />

<strong>and</strong> absent in coarse-grained foliated rock (fig. 3).<br />

In some gneissic kyanite-quartz rock <strong>the</strong> layers <strong>of</strong><br />

kyanite are less uniform, <strong>and</strong> <strong>the</strong> crystals are not<br />

so well oriented (fig. 4). In <strong>the</strong> occurrences just<br />

Content <strong>of</strong> principal minerals, as calculated from chemical analyses<br />

*<br />

VB-W SY-87 NG-439 NG-440 f/<br />

<strong>Sillimanite</strong> <strong>and</strong> <strong>and</strong>alusite. ......<br />

52.6<br />

43.7<br />

l -Q2 "<br />

63.3<br />

27.0<br />

" ".48"<br />

8.66<br />

61.9<br />

37.0<br />

".60"<br />

53.8 1 -^t<br />

43 . 1<br />

1.46<br />

K<br />

8<br />

.......... «C<br />

Total. ..................<br />

97.32<br />

99.44<br />

99.5<br />

98.36 V<br />

1 Includes about 4 percent topaz, as determined by point-counter method<br />

<strong>of</strong> analysis <strong>of</strong> 6 thin sections.<br />

Mode<br />

NG-437<br />

NG-437<br />

40<br />

3<br />

40<br />

17<br />

<strong>and</strong> zircon<br />

Total. ...................<br />

Minor<br />

100<br />

FIGURE 2. Photomicrograph <strong>of</strong> kyanite quartzite from crest <strong>of</strong> Crowders<br />

Mountain, Gaston County, N.C. Shows typical anhedral habit <strong>of</strong> much <strong>of</strong><br />

<strong>the</strong> kyanite (k) in <strong>the</strong> district. Opaque mineral is pyrite. O<strong>the</strong>r minerals<br />

are quartz (q) <strong>and</strong> limonite-stained white mica (m). Plane-polarized light.

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