“…Complete Feleaching resulted in a pure-TiÛ2 phase, usually anatase, similar to that observed in tropical weathering conditions in which humic acids contribute to iron leaching . Sutton paleoplacers were subjected to such conditions during Cambrian time ; Fig could not explain the locally abundant rutile, which usually occurs at high pressure and temperature (Shannon and Pask, 1964;Goldsmith and Force, 1978; , 1961;Heald and Weiss, 1972;Eppler, 1987). However, Gribb and Banfield (1997), Penn and Banfield (1999), Zhang and Banfield (1999) have demonstrated experimentally that rutile can crystallize from nanocrystalline anatase, similar to that found in the Sutton deposits, under hydrothermal conditions.…”