CAJ | 학술논문

通过井下的详细勘查和显微镜下鉴定，对广西龙湾铅锌矿床的矿石组构特征进行了系统研究.矿区矿石构造主要为块状构造、浸染状构造、网脉状构造和斑杂状构造；结构主要为结晶作用和交代作用形成的结构，其次为固溶体分离作用、结晶物质重结晶作用和压力作用形成的结构.同时将成矿期次分为沉积成岩期、中低温热液成矿期和表生氧化期，其中热液成矿期是矿床的主要成矿期.根据矿物组合特征，将成矿划分为五个成矿阶段，分别是黄铁矿-石英-方解石阶段、闪锌矿-方铅矿-黄铁矿阶段、黄铁矿-闪锌矿-方铅矿-黄铜矿阶段、石英-方解石阶段、氧化物阶段.矿物的生成顺序为黄铁矿1-闪锌矿（黄铜矿1）-方铅矿-黄铁矿2-黄铜矿2.最终确定龙湾矿床为受构造活动控制的中低温热液充填交代-叠生改造型多金属矿床.
통과정하적상세감사화현미경하감정，대엄서룡만연자광상적광석조구특정진행료계통연구.광구광석구조주요위괴상구조、침염상구조、망맥상구조화반잡상구조；결구주요위결정작용화교대작용형성적결구，기차위고용체분리작용、결정물질중결정작용화압력작용형성적결구.동시장성광기차분위침적성암기、중저온열액성광기화표생양화기，기중열액성광기시광상적주요성광기.근거광물조합특정，장성광화분위오개성광계단，분별시황철광-석영-방해석계단、섬자광-방연광-황철광계단、황철광-섬자광-방연광-황동광계단、석영-방해석계단、양화물계단.광물적생성순서위황철광1-섬자광（황동광1）-방연광-황철광2-황동광2.최종학정룡만광상위수구조활동공제적중저온열액충전교대-첩생개조형다금속광상.
Ore-fabric characteristics of Pb-Zn deposit systematic study in Longwan,Guangxi by detailed exploration of mine and the microscopic identification. Ore structure is mainly massive structure,dissemination structure,stockwork structure and taxitic structure. The texture is mainly formed in metasomatism and crystallization ,secondly for solid solution separation,crystallized matter recrystallization and pressure effect. Mineralization periods into sedimentary diagenesis,in epithermal mineralization period and supergene oxidation stage,the hydrothermal mineralization period mainly is the deposit metallogenic period. According to the characters of mineral composition,the mineralization is divided into five stages of mineralization,which is pyrite-quartz-calcite stage,sphalerite-galena-pyrites stage, pyrite-sphalerite-galena-chalcopyrite stage,quartz-calcite stage,oxide stage.Mineral equence is pyrite 1-sphalerite (chalcopyrite1)-galena-pyrite 2-chalcopyrite2. It is determined that Longwan ore deposit is low-temperature hydrothermal filling account-storeyed reworked polymetallic deposits control by tectonic activity.