Structure: | Ne Trending Shears And Schultze Granite Dikes Throughout Area. Precambrian Madera Diorite Outcrops 1/2 Mile E Of Mine, Shear Zone Is Parallel To Schist Bedding-Foliation, But Has Discordant Dip To The Sw, Ore Ends In Minor Premineral Cross Fault. Offset Segment Is Only Slightly Mineralized. Granite Dikes Parallel To Shear Zone Both 1/2 Mile N And 1/2 Mile S |