黑龙江东安金矿床地质地球化学特征初探  

The geology and geochemistry of the Dongan Gold Deposit in Heilongjiang Province

作　　者：薛明轩[1] 叶松青[2] 刘智明[1] 杨增武[3] 郭继海[1] 苏仁奎[1] 陈海明[1] 

机构地区：[1]黑龙江省有色金属地质勘查七0七队 [2]吉林大学 [3]黑龙江省有色金属地质勘查七0二队

出　　处：《黄金》2002年第7期1-3,共3页Gold

摘　　要：东安金矿床是黑龙江省新近发现的具大 -特大型远景的浅成热液金矿床。受断裂和隐爆角砾岩带控制 ,赋存于中生代中酸性火山 -侵入岩及晚印支期碱长花岗岩强硅化带中 ,成矿与火山 -侵入岩作用有密切成生关系。成矿物质主要来源于火山 -侵入岩 ;成矿温度14 4～ 348℃ ;成矿深度约 0 .2～ 1.0km ;成矿时代为中燕山晚期。As a newly found deposit in Heilongjiang, Dongan gold deposit has a large super potential and belongs to the epithermal gold deposit. Controlled by the fault and alloclastic breccia, the deposit exists in the silicon alternation zone of the intermediate acidity intrusive rock in Mesozoic era and the late Indo china epoch alkali feldspar granite,the formation of deposit is closely associated with the volcano intrusive action.The volcano intrusive rock is the most important ore forming material.The metallogenic temperature from 144℃ to 348℃. The metallogenic depth is 0.2～1.0km. The deposit were formed in the late middle Yanshanian period.

关 键 词：地质地球化学特征 黑龙江 东安金矿床 

分 类 号：P618.51[天文地球—矿床学]