“…Systematic zoning of the garnetite with its surrounding rocks, the relatively coarse-to mediumgrained garnets themselves ( fig. 14), their occurrence In a high-temperature hydrothermal environment (Theodore and Blake, 1975), and their overall petrologic similarity to many other similar rocks in or near porphyry copper deposits that replace carbonate (Ransome, 1904;Lindgren, 1905;Knopf, 1918;Spencer, 1917;Gale, 1965;Moolick and Durek, 1966;Eastlick, 1968;James, 1971;Himes, 1972; and many others) all suggest to us these rocks grew in part at the expense of some carbonate. Certainly there is some textural evidence that garnet and pyroxene at Copper Canyon may have grown from a carbonate-rich host.…”