河北省兴隆县太平村钼矿地质特征及成矿潜力评价  

Geological features and metallogenic potential evaluation of Taipingcun Mo deposit of Xinglong County,Hebei Province

作　　者：杨玉山[1] 刘剑波[1] 宋海峰[2,3] 聂卫东[1] 张金江[1] 孙金龙[1] 侯建伟[1] 

机构地区：[1]河北省地矿局秦皇岛矿产水文工程地质大队,河北秦皇岛066001 [2]长春工程学院勘查与测绘学院,吉林长春130061 [3]吉林大学地球科学学院,吉林长春130021

出　　处：《吉林地质》2012年第1期46-48,87,共4页Jilin Geology

摘　　要：位于华北板块北缘的燕辽成矿带中已发现了多处钼(铜)矿床(点),兴隆县太平村钼矿位于燕辽成矿带中部,矿区内构造发育、岩浆活动频繁,具有多期岩浆热液活动特征,具有较好的找矿前景。目前所发现的钼(铜)矿床(点)多位于密云—青龙断裂北侧,而太平村钼矿位于该断裂南侧,该矿床的发现对密云—青龙断裂南侧寻找钼矿具有指导意义。Many Mo（Cu） deposits（spots） have been discovered in Yanliao metallogenic belt,on the north margin of North China plate.Taipingcun Mo deposit of Xinglong County is located in the central part of Yanliao metallogenic belt.The faulted structure is extremely well-developed in the mining area and the magmatic activities are frequent,showing a characteristic of multi-episode magmatic hydrothermal activities.These characteristics suggest preferable prospecting potential for ore field.Mo（Cu） deposits（spots） founded so far lie to the north of Miyun-Qinglong fault concentrately,while the Taipingcun Mo deposit lies to the south of the fault.Thus,the discovery of Taipingcun Mo deposit puts forward instructive suggestions for prospecting exploration of Mo deposit in southern area of Miyun-Qinglong fault.

关 键 词：兴隆县 太平村钼矿 成矿流体 燕辽成矿带 

分 类 号：P618.65[天文地球—矿床学]