The Upper Triassic intrusions of the Big Kidd complex are consanguineous with property volcanics, having intruded their own volcanic pile. The alkaline complex features intrusives of monzonite, monzodiorite, diorite, and syenomonzonite composition, hosted within intermediate-mafic volcanic flows, tuffs and volcaniclastics. Intrusions trend southeast, with the elliptical Big Kidd breccia body exposed over aroughly 300 x 600-meter area. The breccia pipe is believed to represent a sub-verticalvolcanic neck dominated by fragments of Nicola Group volcanics and microdiorite to microsyenodiorite, and monzonite to syenomonzonite intrusives.The property straddles a triple fault junction of the Kentucky-Alleyne, Allison and Quilchena faults.West to southwest trending faults have been interpreted to lie between the Big Kidd and Big Siouxtargets and represent areas of increased alteration and fluid flow.
Qualified Persons
Scott Dorion, B.Sc, P.Geo., technical advisor to the Company, is the Qualified Person as defined by National Instrument 43-101 who has reviewed and approved the technical information on this website page.