Changes in the host rocks of the Zyryanovskoe deposit
Authors:
Abstract
All available samples contain, in greater or lesser quantities inclusions of ore minerals: pyrite, zinc blende and partly galena. This clearly indicates that they were taken in the immediate vicinity of the ore body. The spatial location of these samples is evident from the accompanying diagram. As is known, the Zyryanovskoe deposit constitutes a rather irregularly branched gelatinous mass.
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References
- Metasomatic Processes in Fissure-Veins; cited from a reference in Z. f. prakt. Geol. 1901. p. 232.
- Rosenbusch — Elemente der Gesteinslehre. 1910. p. 557.
- K. I. Bogdanovich — Kurs rudnykh mestorozhdenii [Course on Ore Deposits]. p. 266.
- Geologicheskie Issledovaniia v Revdinskom, Verkh-Isetskom i Murzinskom raionakh [Geological Investigations in the Revda, Verkh-Isetsk, and Murzinka Districts]. pp. 122–123 and Plate XXV, Fig. 99.
- Zur Kenntniss einiger Sericitgesteine, welche neben und in Erzlagerstätten auftreten [On the Knowledge of Some Sericite Rocks Which Occur Adjacent to and Within Ore Deposits]. Neues Jahrbuch für Mineralogie, Geologie und Paläontologie. 1883. Vol. II, Beilage B.
- The gold and silver veins of Silver City, de Lamar and other mining districts in Idaho. Annual Report of the United States Geological Survey. 1898–99, Part III, specifically pp. 218–231.
- Lindgren — Metasomatic Processes.