CAJ | 학술논문

渣滓溪锑钨矿区赋矿地层均为五强溪上段，矿体主要赋存于F3的上盘，有编号的辉锑矿脉共计有77条，工业矿体47条；按与F3距离分为Ⅰ、Ⅱ、Ⅲ脉组，以Ⅰ脉组含矿最佳，Ⅱ脉组次之，Ⅲ脉组含矿性较差。系统总结了渣滓溪锑钨矿区矿化富集规律，结果表明，矿脉成组成带分布，整体呈南东侧伏规律；矿脉明显交汇富集，在倾向上倾角变缓及构造膨胀部位富集，主脉富集程度与F3密切相关；赋矿岩系具有锑钨组合特征，锑钨成生关系反映在各自的矿体赋存于不同序次的断裂中；锑矿脉走向与钨矿层走向近于直交，为锑钨叠加成矿的异体共生矿床。渣滓溪锑钨矿区上部锑钨资源共生，资源的开发潜力巨大。
사재계제오광구부광지층균위오강계상단，광체주요부존우F3적상반，유편호적휘제광맥공계유77조，공업광체47조；안여F3거리분위Ⅰ、Ⅱ、Ⅲ맥조，이Ⅰ맥조함광최가，Ⅱ맥조차지，Ⅲ맥조함광성교차。계통총결료사재계제오광구광화부집규률，결과표명，광맥성조성대분포，정체정남동측복규률；광맥명현교회부집，재경향상경각변완급구조팽창부위부집，주맥부집정도여F3밀절상관；부광암계구유제오조합특정，제오성생관계반영재각자적광체부존우불동서차적단렬중；제광맥주향여오광층주향근우직교，위제오첩가성광적이체공생광상。사재계제오광구상부제오자원공생，자원적개발잠력거대。
Ore-bearing strata in Zhazixi antimony tungsten mining area are all in upper Wuqiangxi ,the ore body mainly occurs in the hanging wall of the F 3 ,stibnite veins number a total of 77 ,and the common industrial ore bodies are 47;according to the distance away from F 3 ,Ⅰ,Ⅱ,Ⅲvein groups are classified .GroupⅠis the best in ore-bearing potentials,II vein group poorer and group Ⅲore veins poorest.The regularity of mineralization Zhazixi antimony tung-sten mining area is systematically summarized .The results show thatveins distribute in groups and belts ,laterally tren-ding SE on the whole;veins enrich in the intersection ,where inclination angle slows ,and in the tectonic expansions;the enrichment degree of main veins is closely related with F 3;the ore-bearing rock systemtakes on combined features of antimony and tungsten ,and the mineralization relation between antimony and tungsten are reflected by the fact that their respective orebodies occur in fractures of different sequence; the trending of antimony veins and tungsten strata cross each other nearly orthogonally ,indicating a symbiosis deposit of combined antimony and tungsten mineralization . There is symbiosis of antimony and tungsten in upper Zhazixi mining , suggesting great resource development poten-tials.