Epithermal Low Sulfidation Au-Ag Deposits
![]() Epithermal deposits are divided into high sulfidation (HS) and low sulfidation (LS) types. The HS deposits occur in leached silicic rocks and are characterized by highly acidic fluids, whereas the LS deposits are characterized by reduced fluids of neural pH. Common minerals associated with epithermal deposits include microcrystalline, drusy quartz or colloform silica, illite, smectite, and adularia. Specular hematite occurs at some depth and goethite occurs near or at the surface. |
Charay property, Sinaloa, Mexico. MUSGROVE MINERALS CORP.
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