“…During geologic mapping in the Lynn window and vicinity in 1968-71, 877 samples of mineralized hydrothermally altered and unaltered sedimentary, igneous, and metamorphic rocks ranging in age from Cambrian to Tertiary were collected for chemical analysis by J. G. Evans. The analyses were published by Evans and Peterson (1980). All the samples were analyzed for 29 elements (Ag, As, B, Ba, Be, Bi, Ca,…”