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A N T I M O N Y : ITS HISTORY, CHEMISTRY, MINERALOGY ...

A N T I M O N Y : ITS HISTORY, CHEMISTRY, MINERALOGY ...

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48 THE METALLURGY OF ANTIMONY.<br />

stibnite, sometimes associated with iron pyrites and brown spar, is<br />

found in true veins, or between the planes of stratification, or in<br />

cleavage fissures. This is a good example of the lateral immigration<br />

of antimony ore from fissures into and along beds of shaly rocks. (C.)*<br />

At Bohmsdorf and Wolfsgalgen, near Schleiz, stibnite is found in<br />

quartz veins traversing palaeozoic schists. The subsidiary minerals<br />

are zinc-blende, plumose stibnite, pyrophyllite, and iron spar. (A.)<br />

At Mobendorf, antimony ore occurs in veins, cutting the gneiss<br />

formation, with fillings of stibnite and some berthierite, bournonite,<br />

striated kaolin, steinmannite, zincite, kermesite, stibiconite, pyrite,<br />

quartz, and brown spar. At Braunsdorf, a few kilometres off, the<br />

same ore is found intimately associated with rich silver ores. In the<br />

vicinity of Freiberg, the quartz-stibnite vein is simply the continuation<br />

of a true quartz formation. For this reason Freiesleben called<br />

it the " Mobendorf Formation ;; (A).<br />

Summary.<br />

Mobendorf<br />

Hayniclien (Niedersteigis)<br />

Ennersdorf , r, . n. o , . ,<br />

Seiferdorf f Gryrtalkne Schist<br />

Rochlitz<br />

Schoneck<br />

Brandholz<br />

"Wolfsberg Silurian.<br />

Goesdorf Lower Devonian.<br />

Arnsberg Culm.<br />

HUNGARY.<br />

At Magurka, according to von Cotta, the granite is traversed by<br />

many quartz veins, varying from a few centimetres to 4 m. in thickness.<br />

They carry stibnite and free gold, enclosing sometimes some of the<br />

country. The accessory minerals found in these veins are galena,<br />

zinc-blende, pyrite, copper pyrite, brown spar, and calc-spar.<br />

Ordinarily the quartz occurs along the walls of the veins, while<br />

the stibnite occupies the central part. (B.)<br />

At Pricov, near Selcan, stibnite is found, according to A. Hoffmann,<br />

in veins of hornstone, generally accompanied by kersantite dykes,<br />

cutting through the granite. At a depth of 18 m. (59 ft.) the<br />

stibnifce is decomposed to stibiconite. (A.)<br />

Some of the veins carrying antimony ores in the Rechnitz<br />

* By some authors this is classified under E.

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