“…A number of other deposit types are either spatially, temporally, or genetically related to alkalic-type epithermal gold deposits. The most common types of associated deposits include (1) copper, iron, gold, and zinc-rich skarns, such as those in New Mexico (McLemore, 1996), deposits near Galore Creek (Enns and others, 1995), and many in Montana (Woodward and Giles, 1993); (2) polymetallic replacement deposits (Ag, Pb, Zn, Cu, Au), the best example of which is the Kendall deposit in Montana (Lindsey, 1985); (3) fluorspar vein and breccia deposits and tungsten-bearing veins, exemplified by deposits in Boulder County (Kelly and Goddard, 1969;Nash and Cunningham, 1973); and (4) local carbonatites (REE, Nb), for example in New Mexico (McLemore, 2010). The presence of these deposits does not necessarily indicate the existence of nearby alkalic-type epithermal deposits, nor does their absence preclude the occurrence of nearby alkalic-type epithermal gold deposits.…”