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综合运用遥感微差信息处理技术、水系沉积物X荧光测量和地表基岩伽玛能谱测量方法研究了山西堡子湾金矿的成矿流体场 ,发现主要的矿化蚀变带呈NW向展布 ,与含矿的NEE向角砾岩带斜交 ,表明成矿后受到一定程度的改造。矿区内存在着两类矿体 ,即陡倾斜的隐爆角砾岩型金矿和缓倾斜的蚀变岩型金矿 ,已知矿体和蚀变带主要受矿区南部的环形构造控制 ,该环形构造可能与隐伏岩体顶部拆离断层系统有关
Based on the application of remote sensing data processing technology, X-ray fluorescence measurement of sediments and surface bedrock gamma spectrometry, the ore-forming fluid field of the Baoziwan gold deposit in Shanxi Province is studied. The main mineralized alteration zones are NW-spread Cloth, oblique to the ore-bearing NEE-breccia zone, indicates some degree of alteration after mineralization. There are two types of ore bodies in the mining area, namely, steeply inclined cryptoexplosive breccia type gold deposits and gently inclined altered rock type gold deposits. The known ore bodies and alteration zones are mainly controlled by the ring structure in the southern part of the ore area. The structure may be related to the detachment fault system at the top of the concealed rock mass