1989 Annual report

Abstract

Several styles of mineralisation occur at Gandy's Hill within the bulk of the mineralisation occurring within siltstones. The styles include A) Saddle Reef, B) stockwork veining across the anticline, C) narrow quartz veins peripheral to the axis and D) fault related mineralisation. Two saddle reefs are observed at Gandy's Hill, they are Gandy's Hill and North Gandy's Hill Reef. North Gandy' s Hill Reef has gold grades ranging from 1.0 to 12.0g-t At South Gandy's mineralisation is hosted in a stockwork zone with grades ranging from 1.0 to 15.0g-t.