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黄铁矿的电性与成矿条件有关,并可作为各种成因金矿化的标志。本文所述的含金硫化物建造和含金硅质建造的矿床赋存在缝合的裂谷构造的边缘部位。地层为(自下而上):火山-白云质-硅质建造;硅质-陆源建造;陆源(亚复理石)建造;碳酸盐类白云质-灰质建造以及磨拉石(火山磨拉石)建造。在早期迥返阶段,形成火山-滑动沉积(硬砂质)建造;在后期迥返阶段,侵入有岩基型钾(钠-钾)质花岗岩类岩体以及杂质脉岩群。主要成矿围岩为陆源、滑动沉积建造。矿化受与裂谷冰川槽大体平行及近于对角线方向分布的深断裂长期活动带所控制,并为平缓推覆构造所屏蔽。
The electrical properties of pyrite are related to metallogenic conditions and can be used as a sign of gold mineralization for various reasons. The gold-bearing sulphide-bearing and gold-bearing siliceous deposits described in this paper are located at the margin of stitched rift structures. The strata are (bottom-up): volcano-dolomitic-siliceous construction; siliceous-terrigenous construction; terrigenous (subboundary) construction; dolomitic carbonate-gray matter formations and molasse )put up. In the early stage of relict, volcano-slip sediments (hard sandy) were formed; in the later stage of relict, intrusive rocks were rock-basal type potassium (sodium-potassium) granites and intrusive rocks. The main metallogenic rock is terrestrial, slip sedimentary construction. Mineralization is dominated by the deep-fault long-term activity belt distributed roughly parallel to and nearly diagonal to the rift glacier trough and is shielded by the gentle nappe structure.