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

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

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Paragonite.<br />

Margarite.<br />

VB-116a...<br />

VB-116b. . .<br />

VB-116a: Typical<br />

colorless mica with<br />

good micaceous<br />

cleavage.<br />

VB-116b: Colorless<br />

bundles <strong>of</strong> fibers <strong>and</strong><br />

poorly defined plates<br />

with a slight waxy<br />

luster.<br />

1.48<br />

2.1<br />

.79<br />

5.22<br />

5.6<br />

4.9<br />

O.OX percent<br />

Li.<br />

1 . 6 percent Ca .<br />

4 . 9 percent Ca ;<br />

0 . X percent<br />

Li.<br />

Paragonite; film No.<br />

6880. By F. A.<br />

Hildebr<strong>and</strong>. 4<br />

Paragonite plus muscovite<br />

<strong>and</strong> minor<br />

kaolinite. By H.<br />

S. Yoder, Jr.<br />

Margarite. By H. S.<br />

Yoder, Jr.<br />

1.595<br />

3 1 . 604<br />

1.613<br />

3 1.604<br />

1.618<br />

0-5°<br />

325°<br />

Chemical analyses<br />

by J. M. Dowd<br />

<strong>and</strong> J. D.<br />

Fletcher.<br />

Chemical analyses<br />

by P. L. Elmore.<br />

Chemical analyses<br />

by P. L. Elmore<br />

<strong>and</strong> J. D.<br />

Fletcher.<br />

1 X-ray powder camera method used by D. H. Richter, F. A. Hildebr<strong>and</strong>, <strong>and</strong> J. M. Axelrod.<br />

X-ray diffractometer method used by H. S. Yoder, Jr.<br />

2 See complete chemical analysis in table 5.<br />

3 Approximate.<br />

4 The absence <strong>of</strong> muscovite <strong>and</strong> kaolinite in this material suggests that it was not identical<br />

with material analyzed by H. S. Yoder, Jr.<br />

CO?<br />

quartz (fig. 8). dant inclusions<br />

quartz <strong>and</strong> rock are unoriented some abun- contain aggregates. <strong>Kyanite</strong> crystals kyanite-<br />

nonfoliated in ing rock, may irregular<br />

network<br />

<strong>the</strong><br />

form it<br />

kyanite may rock, irregular stringers occur<br />

form- (fig. 7).<br />

kyanite-quartz Mountain In nonfoliated strongly kyanite quartzite is in foliated Willis<br />

principal kyanite occurrence lenses <strong>of</strong> massive kyanite many length. lenses <strong>of</strong> massive feet in The kyanite crystals (fig. 6),<br />

few inches across or (fig. 5), r<strong>and</strong>omly <strong>the</strong> foliation clusters <strong>of</strong> oriented aggregates radiating crystals <strong>of</strong> conformable to generally only nite, across, inches found few are pure kya- through Aggregates nearly <strong>the</strong> rock. <strong>of</strong><br />

deposits. <strong>Kyanite</strong> may in some form coarse-tufted<br />

described, kyanite uniformly<br />

distributed ra<strong>the</strong>r<br />

(h). (r) ; Rutile holes section Crossed in nicols.<br />

coarsely crystalline quartz (q) (k) gneissic <strong>and</strong> characteristic<br />

structure. County,<br />

well-developed kyanite crystals Prince Edward Va. Shows bladed<br />

Photomicrograph kyanite quartzite Mountain, FIGURE 3. <strong>of</strong> from Baker<br />

._ m ^/i*,w *. -i*"***<br />

ffa s<br />

31<br />

o 3<br />

j» a<br />

f+ CD<br />

«-*3 * ^<br />

r«<br />

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Q<br />

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r<br />

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VI

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