“…They note that adularia alteration can occur in rocks up to >500 m laterally from veins, whereas ammonium (NH 4 ) minerals, when present, have a restricted distribution occurring laterally <100-300 m from veins. In a complementary paper, Barker et al (2019) describe the lithogeochemical signatures of hydrothermal alteration associated with the epithermal Au-Ag deposits of the Waihi area in the Hauraki Goldfield. They note the importance of the K/Al ratio, reflecting adularia alteration, along with other element gains (e.g.…”