CAJ | 학술논문

湖南邓阜仙地区位于南岭钨锡铅锌多金属成矿带湖南段东部北侧，郴州—茶陵北东向钨锡多金属成矿区带北东段北侧。研究从区内地层、构造、岩浆活动入手。总结出岩浆和围岩地层是该区的成矿物质来源，而构造则形成了矿液通道与赋矿空间。最后，在以上研究的基础上，指出下一步该区主要是寻找裂隙型、矽卡岩型和隐伏型矿床。
호남산부선지구위우남령오석연자다금속성광대호남단동부북측，침주—다릉북동향오석다금속성광구대북동단북측。연구종구내지층、구조、암장활동입수。총결출암장화위암지층시해구적성광물질래원，이구조칙형성료광액통도여부광공간。최후，재이상연구적기출상，지출하일보해구주요시심조렬극형、석잡암형화은복형광상。
The Dengfuxian area is located in the east Hunan section of the Nanling tungsten-tin-lead-zinc polymetallic metallogenic belt and in the Northeast section of the Chenzhou-Chaling W-Sn polymetallic metallogenic belt. This paper believes that the ore material was derived from strata as wall rocks and ore-formation was controlled by fracture. Crevice and skarn type of deposits are of perspective.