摘要
高松山金矿床是与火山次火山作用关系密切的浅成低温热液型金矿床，受张性断裂控制，赋存在中生代中酸性火山一次火山岩中，成矿与火山一次火山岩关系密切．其成矿温度为230～300℃，包裹体盐度在0．71％～7．31％，成矿物质来源于火山一次火山岩；成矿流体以大气降水为主。
Gaosongshan gold deposit is of hypothermal type related to volcanism- subvolcanism. The deposit is controlled by tension faults, and occurred in Mesozoic volcanic - subvolcanic rocks, the metallogenic temperature is about 230--300℃, the inclusion salinity is about 0.71% ～7.31%, the metallogenic material is from volcanic ～suhvolcanic rocks, and the metallogenic fluid is mainly the atmospheric water.
出处
《有色矿冶》
2006年第4期1-4,共4页
Non-Ferrous Mining and Metallurgy
