CAJ | 학술논문

桐村斑岩型钼铜矿床位于钦杭成矿带东段。由于其紧邻赣东北大型矿集区，具有良好的成矿地质背景和地质条件。在此前提下，对桐村典型矿床的研究，探讨浙西桐村钼铜矿床的成岩成矿过程及特点。对在浙西地区寻找发现相同类型的大型矿床有着重要的实际意义，对钦杭成矿带浙江段的成矿规律及丰富矿床成矿理论有着重要的理论。
동촌반암형목동광상위우흠항성광대동단。유우기긴린공동북대형광집구，구유량호적성광지질배경화지질조건。재차전제하，대동촌전형광상적연구，탐토절서동촌목동광상적성암성광과정급특점。대재절서지구심조발현상동류형적대형광상유착중요적실제의의，대흠항성광대절강단적성광규률급봉부광상성광이론유착중요적이론。
TongCun porphyry molybdenum copper deposit is located in the eastern of Qin-Hang metallogenic belt. The study area is close to ore concentrating area of north east JiangXi Province and have excellent geology mineralization condition. Focus on the tectonic setting of yanshanian magmatic and the diagenesis and mineralization process of TongCun deposit. This area have great resource potential. The study of TongCun deposit is contribute to the recognize of mineralization regularity.