偏岩子金矿的开采起始于清朝,现今遗留古采迹有10余处,曾是西南地区有名的老矿。该研究区北起狮子山,南至跑马山,沿郭达山断裂分布有偏岩子、灯盏窝、新尖子、狮子山、箭杆山、郭达山、清水沟、清水沟果子、滚石坡等10余处金矿床。过去对该矿的成因类型一直认识不清,直到20世纪80年代,通过对偏岩子金矿床矿物流体包裹体的各种测试数据的分析和S、Pb、H、O、C等各种同位素的研究,该矿被 Partial rock gold mining began in the Qing Dynasty, there are now more than 10 legacy mining sites, was once famous in the southwest of the old mine. The study area is from Lion Rock to the north and to Happy Valley from the South. More than 10 gold such as partial rock, lamppost, new eldest son, Lion Rock, Arrow Mountain, Gu Dashan, Qingshuigou, Qingshuigou fruit, Deposits. In the past, the type of genesis of this mine has not been fully understood until the 1980s. Through the analysis of various test data of mineral fluid inclusions in the Piyamizu gold deposit and various isotopes of S, Pb, H, O and C Research, the mine was