Economic Geology; April 2003; v. 98; no. 2;
p. 225-234; DOI: 10.2113/98.2.225
© 2003 Society of Economic Geologists
Part 1. Regional Studies and Epithermal Deposits
David A. John
U.S. Geological Survey, MS-901, 345 Middlefield Road, Menlo
Park, California 94025
Albert H. Hofstra
U.S. Geological Survey, MS-973, Federal Center, Denver,
Colorado 80225
Ted G. Theodore
U.S. Geological Survey, MS-901, 345 Middlefield Road, Menlo
Park, California 94025
Corresponding author: e-mail, djohn@usgs.gov
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Introduction
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Northern Nevada is one of the Earths premier gold- and
silver-producing regions, and gold and silver are mined from a wide range of
deposit types (Table 1). Current production largely comes from Carlin-type
sedimentary rock-hosted disseminated gold deposits (Christensen, 1995; Teal and
Jackson, 1997; Bettles, 2002), many of which lie along linear trends (Fig. 1;
Roberts, 1960, 1966; Berger and Bagby, 1991). The small area of the Carlin trend
(approximately 8 x 65 km) is North Americas most prolific gold mining
district, producing nearly 125 t (4 Moz) of gold annually. Since large-scale
mining began in 1965 with the opening of the Carlin mine, the Carlin trend has
produced more than 1555 t (50 Moz) of gold. During 2001, gold production from
the entire state of Nevada was nearly 253 t (8.13 Moz), which accounted for
approximately 76 percent of the United States and 10 percent of the world
production (Price and Meeuwig, 2002). In 2001, only the countries of South
Africa and Australia produced more gold than the state of Nevada. In addition,
Nevada produced 543 t (17.4 Moz) of silver in 2001about 31 percent of the
United States production and 3 percent of the world production.
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TABLE 1 TABLE 1. Major Types and Examples of Gold Deposits in Northern
Nevada
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FIG. 1. Index map of northern Nevada showing significant Carlin-type, pluton-related,
and epithermal gold deposits (modified from Long et al., 1998), and geographic
features and deposits described in the text. Heavy lines show the major mineral
trends and lineaments. Small box at north end of the Carlin trend shows the
location of the Beaver Peak and Santa Renia Fields 7 minute quadrangles
(Theodore et al., 2003). Dashed lines outline the corridor . . . [Full Text of this Article] |
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