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rare earth elements in Wyoming

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figure 26. Dahllite concretions from the Cretaceous Thermopolis<br />

Shale near the Wyoben bentonite m<strong>in</strong>e, northwest of Greybull.,<br />

A, sample 20121018JC-E. B, <strong>in</strong>terior of a dahllite concretion.<br />

sta<strong>in</strong>ed ve<strong>in</strong> quartz, m<strong>in</strong>eralized with chalcopyrite,<br />

pyrite, bornite, malachite, and hematite, analyzed<br />

for this report yielded 17.25 ppm (0.50 oz/ton)<br />

gold, 41.3 ppm (1.20 oz/ton) silver, and 2.62<br />

percent copper.<br />

Gold Co<strong>in</strong> M<strong>in</strong>e, SW¼ sec. 11, T. 15 N., R. 87<br />

W., Southern Carbon County<br />

63<br />

The Gold Co<strong>in</strong> m<strong>in</strong>e targeted copper, lead,<br />

gold, and silver m<strong>in</strong>eralization with<strong>in</strong> a 0.3<br />

m (1.0 ft) wide quartz ve<strong>in</strong> (Beeler, 1902;<br />

Hausel, 1997). The ve<strong>in</strong> is concentrated<br />

with<strong>in</strong> a fissure that trends 75˚ and dips to<br />

the south at a high angle (Spencer, 1904).<br />

The ve<strong>in</strong> cuts the regional foliation of the<br />

host<strong>in</strong>g Late Archean black diorite (Beeler,<br />

1902; Spencer, 1904). A sample of ve<strong>in</strong><br />

quartz with abundant limonite (possibly replac<strong>in</strong>g<br />

sulfides), galena, chalcopyrite with<br />

chalcocite rims, and m<strong>in</strong>or malachite (Sample<br />

20121203WSGS-B) from the Gold<br />

Co<strong>in</strong> m<strong>in</strong>e yielded 318 ppm (9.27 oz/ton)<br />

silver, 0.11 ppm (0.003 oz/ton) gold, 0.11<br />

percent copper, and 14.6 percent z<strong>in</strong>c.<br />

Section 8 M<strong>in</strong>e, S½SE¼ sec. 8, T. 14 N.,<br />

R. 85 W., Southern Carbon County<br />

The Section 8 m<strong>in</strong>e targeted copper<br />

m<strong>in</strong>eralization hosted <strong>in</strong> pyritized banded<br />

chert with<strong>in</strong> amphibolite of the Silver<br />

Lake Metavolcanics, though the exact<br />

field relationship between the amphibolite<br />

and chert is unknown. In addition to the<br />

amphibolite, chlorite garnet schist is also<br />

present <strong>in</strong> the Silver Lake Metavolcanics<br />

<strong>in</strong> the vic<strong>in</strong>ity of the Section 8 m<strong>in</strong>e. The<br />

banded chert has a trend of 81˚ and dips<br />

52˚ SE. M<strong>in</strong>eralization is concordant with the local<br />

band<strong>in</strong>g <strong>in</strong> the chert. A sample from the m<strong>in</strong>e<br />

yielded 2.61 percent copper but no detectable gold<br />

(Hausel, 1986; 1997); no silver was reported. A<br />

sample of pyrite- and chalcopyrite-bear<strong>in</strong>g banded<br />

chert (Sample 20121203WSGS-D) yielded 27.4<br />

ppm (0.80 oz/ton) silver and 6.75 percent copper.<br />

table 22. Concentration of the REE, P 2 O 5 , uranium, and thorium <strong>in</strong> dahllite concretions from the Thermopolis Shale<br />

near Greybull. Bold values <strong>in</strong>dicate concentrations greater than five times crustal abundance.<br />

Element La (ppm) Ce (ppm) Pr (ppm)<br />

Wyo-Ben m<strong>in</strong>e dahllite<br />

Nd (ppm) Sm (ppm) Eu (ppm) Gd (ppm) Tb (ppm) Dy (ppm) Ho (ppm)<br />

20121018JC-E 65.4 135 20.1 93.2 24.4 6.32 31.9 4.83 26.7 4.96<br />

Element Er (ppm) Tm (ppm) Yb (ppm) Lu (ppm) Sc (ppm) Y (ppm) Cumulative<br />

REE (ppm)<br />

P O (%) 2 5 U (ppm) Th (ppm)<br />

20121018JC-E 10.8 1.15 5.56 0.72 9 187.5 627.5 33.6 3.75 1.03

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