CAJ | 학술논문

矿床位于马兰峪复背斜核部即冀东中部侵入岩带西段，钼矿化主要发育在太古宙变质岩、角砾岩及中生代二长花岗岩内，矿脉呈细脉状、浸染状产出，目前初步控制的远景储量有望达到大型以上。通过对该矿床找矿经验、成矿地质特征、物化探异常特征和找矿标志等进行总结，经对比分析发现，区内其它几个中生代花岗岩西侧的钼异常，同样具有较好的找矿前景。该矿床的发现不仅对在冀东马兰峪复背斜核部寻找大型钼矿具有重要的指导意义，而且对促进区域成矿理论与成矿规律的研究，都具有重要的理论与实际意义。
광상위우마란욕복배사핵부즉기동중부침입암대서단，목광화주요발육재태고주변질암、각력암급중생대이장화강암내，광맥정세맥상、침염상산출，목전초보공제적원경저량유망체도대형이상。통과대해광상조광경험、성광지질특정、물화탐이상특정화조광표지등진행총결，경대비분석발현，구내기타궤개중생대화강암서측적목이상，동양구유교호적조광전경。해광상적발현불부대재기동마란욕복배사핵부심조대형목광구유중요적지도의의，이차대촉진구역성광이론여성광규률적연구，도구유중요적이론여실제의의。
The deposit is located in the Malanyu anticlinorium, which is the west of the middle of Eastern Hebei intrusive rock belt. The molybdenum mineralization is mainly formed in the Archean metamorphic, breccia and the Mesozoic monzonitic granite, in veinlets, disseminated output. At present, the scale under control is prospective to be more large-scale reserve. Through the research of the prospecting experiences, metallogenic features, the abnormal characteristics of geophysics and geochemistry, indicator for prospecting, we found that there are better exploration prospects of Mo anomalies of the Mesozoic granite in this area. The discovery and research of Taipingcun Mo deposit have great importance guiding significance to find large molybdenum deposit in Malanyu anticlinorium, and to develop regional metallogenic theory and the regularity.