“…Massive contact metamorphic rocks will affect the circulation of later stage hydrothermal fluids through decreased permeability of the environment surrounding the pluton. (Hudson and others, 1981;Ashleman and others, 1997), Burroughs Bay (Hudson and others, 1981), Malala (van Leeuwen and others, 1994), Endako (Whalen and others, 2001), Kitsault (Steininger, 1985), Canicanian (Knittel and Burton, 1985), MAX (Lawley and others, 2010), Thompson Creek (Hall and others, 1984), altered rocks from Red Mountain (Brown and Kahlert, 1995), Little Boulder Creek (Mutschler and others, 1981), and Cannivan Gulch (Mutschler and others, 1981 …”