该矿于1979年初发现,为配合勘探,同年底投入电法工作。从各种方法得到的成果看,在已知含金的断裂挤压破碎带上获得明显的视电阻率异常,取得了一定的地质效果。 一、矿区地质概况 矿区位于本省著名的上虞——龙泉隆起带的北东段北侧,绍兴——江山深大断裂带 The mine was discovered in early 1979, in line with exploration, the same year put into electric law. According to the results obtained from various methods, obvious apparent resistivity anomalies are obtained on the fractured crushed belt with known gold content and a certain geological effect has been achieved. First, the mining geology Overview mining area is located in the province’s famous Shangyu - Longquan uplift north of the northern section of Shaoxing - Jiangshan deep fault zone