These intersections are all from unaltered, biotitic coarse-grained granitic dykes cutting mafic rocks.    From Wordnik.com.  [StreetInsider.com News Articles] Reference

North of the fault, mineralization is hosted in both porphyry dykes and schistose, carbonatized and biotitic ultramafic rocks north.    From Wordnik.com.  [StreetInsider.com News Articles] Reference

The gold mineralization comprises multiple subvertical, tabular subzones hosted both in silicified greywackes of the Pontiac Group south of the fault contact and in schistose, carbonated and biotitic ultramafic rocks north of the fault contact.    From Wordnik.com.  [Marketwire - Breaking News Releases] Reference

(core length) in a strongly altered diorite (biotitic-calcite-chlorite).    From Wordnik.com.  [Marketwire - Breaking News Releases] Reference