CAJ | 학술논문

提凤太矿集区是秦岭重要的铅锌金多金属成矿区之一，双王金矿是该成矿区中典型的角砾岩型金矿床。本文采用格里戈良提出的原生晕分带指数法，详细研究了双王金矿床KT9矿体和KT8矿体中ZK18-5、ZK30-1和ZK40-53个坑内钻孔的原生晕轴(垂)向分带特征，通过各钻孔中原生晕分带指数垂向变化规律、微量元素衬值及地球化学参数分析进行深部矿化预测。结果显示，双王金矿床原生晕轴(垂)向分带序列呈明显的反带现象， ZK18-5中在标高950 m附近矿化程度最好，矿体向深部逐渐尖灭；ZK30-1在标高980 m附近矿化程度最好，其深部预测有串珠状矿体存在，深部矿化前景较好；ZK40-5在标高850 m附近矿化程度最好，预测深部矿体仍有较大规模的延伸，深部矿化前景较好。
제봉태광집구시진령중요적연자금다금속성광구지일，쌍왕금광시해성광구중전형적각력암형금광상。본문채용격리과량제출적원생훈분대지수법，상세연구료쌍왕금광상KT9광체화KT8광체중ZK18-5、ZK30-1화ZK40-53개갱내찬공적원생훈축(수)향분대특정，통과각찬공중원생훈분대지수수향변화규률、미량원소츤치급지구화학삼수분석진행심부광화예측。결과현시，쌍왕금광상원생훈축(수)향분대서렬정명현적반대현상， ZK18-5중재표고950 m부근광화정도최호，광체향심부축점첨멸；ZK30-1재표고980 m부근광화정도최호，기심부예측유천주상광체존재，심부광화전경교호；ZK40-5재표고850 m부근광화정도최호，예측심부광체잉유교대규모적연신，심부광화전경교호。
The Fengtai ore concentration area is an important Pb-Zn-Au metallogenic area in the Qinling Mountains, and the Shuangwang gold deposit is a representative large-sized deposit of auriferous albite breccias type in this area. Based on Gregorian’s zoning index method, the authors studied the vertical zoning characteristics of primary halos at the depth of drill holes ZK18-5, ZK30-1, and ZK40-5 in orebodies KT9 and KT8. By discussing the vertical variation of the zoning rate of primary halos, the graphical method of 3-end-mumber diagram, and the vertical change rules of the geochemical parameter, the authors hold that the orebody indicated by ZK18-5 thins out gradually at the depth, with a higher degree of mineralization at the elevation of 950 m;bead-shaped orebodies may occur at the depth of ZK30-1, with a higher degree of mineralization at the elevation of 980 m;the ore body indicated by ZK40-5 with a higher degree of mineralization at the elevation of 850 m still extends to the depth without pinching out.