CAJ | 학술논문

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。
위우화북판괴북연적연료성광대중이발현료다처목（동）광상（점）,흥륭현태평촌목광위우연료성광대중부,광구내구조발육、암장활동빈번,구유다기암장열액활동특정,구유교호적조광전경。목전소발현적목（동）광상（점）다위우밀운—청룡단렬북측,이태평촌목광위우해단렬남측,해광상적발현대밀운—청룡단렬남측심조목광구유지도의의。
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.