Geologic descriptionDetails about the prospect are unavailable. Most likely, a gold-bearing quartz vein(s) cuts the Late Cretaceous Willow Creek Pluton. The Willow Creek Pluton is a zoned pluton. The outer part consists of hornblende quartz diorite and lesser hornblende tonalite; the core consists of hornblende-biotite granodiorite, and lesser hornblende-biotite quartz monzodiorite and biotite quartz monzonite. |
Geologic map unit |
(-149.242210151643, 61.7994709534638) |
Mineral deposit model |
Low-sulfide Au-quartz veins? (Cox and Singer, 1986; model 36a?). |
Mineral deposit model number |
36a? |
Age of mineralization |
Late Cretaceous or younger; the host of mineralization is the Late Cretaceous Willow Creek Pluton. |