吉林省白山市金英金矿床地质特征及成因探讨  

GEOLOGY AND GENESIS OF THE JINYING GOLD DEPOSIT IN JILIN PROVINCE

作　　者：刘文香[1] 满永路 王兴昌[1] 

机构地区：[1]吉林省有色金属地质勘查局602队,吉林白山134300 [2]吉林省有色金属地质勘查局604队,吉林桦甸132400

出　　处：《地质与资源》2009年第4期279-283,共5页Geology and Resources

摘　　要：金英金矿床产于叠加在先期存在的新元古界钓鱼台组石英砂岩与古元古界珍珠门组硅化白云质大理岩之间的不整合面附近的硅化构造角砾岩带中的F100断裂内,主要受区域性断裂F102及局部性断裂F100的联合控制.金英金矿形成的特殊环境和物化条件,使其具有独特的矿物组合和矿石结构构造,是我国目前发现的一种新类型金矿.金矿类型属于中生代造山带型金矿.The Jinying gold deposit in Baishan City, Jilin Province is tectonically located in the northeastern margin of Liaodong anteclise, Sino-Korean metaplatform. It occurs in the silicified tectonic breccia belt between the Neoproterozoic Diaoyutai quartzose sandstone and the Paleoproterozoic Zhenzhumen silicated dolomitic marble. The orebodies are jointly controlled by the regional fault F102 and local fault F100. The special forming environment and physical-chemical conditions make its unique assemblage of minerals and texture of ores. This deposit belongs to a new type recently found in China, the Mesozoie orogenic type.

关 键 词：金英金矿床 F100断裂 硅化构造角砾岩带 硅化 赤铁矿化 造山带金矿 吉林省 

分 类 号：P615.51[天文地球—矿床学]