Annual report 21 January 1989 to 20 January 1990.

Abstract

Structural features reported include: Howley Anticline. The detailed infill soil sampling programme returned significantly anomalous zones. Gold within the tenement generally occurs in quartz veins parallel to shear fabrics in stockwork zones which occur as tension fractures formed synchronously with shearing and veins also parallel to either bedding or axial plane cleavage. The cross cutting, replacement nature of most of the mineralisation suggests that it post dates the deposit of Finniss River sediments, and the Zamu Dolerite mineralisation appears to be synchronous with shearing and post dates F1 folding.