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Copper and Silver

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Abstract

Sedimentary deposits of copper are common, contributing between 25 and 30 percent of the world’s production (Jacobsen 1975, table 1). Most of this amount, however, comes from one district, the Central African Copperbelt. Silver is almost always associated with the copper in these ores, and so will also be considered in this chapter. Also discussed are supergene deposits of copper and silver. Although of diminished economic importance today, they serve to illustrate the geochemical processes involved in ore-formation without some of the uncertainties associated with interpretations of the genesis of the larger deposits.

Keywords

Black Shale Copper Deposit Ground Water Flow Quartz Arenite Native Copper 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer-Verlag New York Inc. 1983

Authors and Affiliations

  1. 1.Department of Geology, H.N. Fisk Laboratory of SedimentologyUniversity of CincinnatiCincinnatiUSA

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