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欧洲的海西带控制了几处含有一批矿化和一些可开采矿床的金矿区。在对基底有影响的海西晚期变形阶段,形成了许多有经济价值的金的富集。 在成矿的微裂隙中和流体漂移的特定阶段内,含金石英脉型矿化是具有多阶段成矿的特点。微裂隙和流体作用影响到早期沉淀的石英脉的基质。根据包括从区域到显微范围内的构造研究以及对矿物组合、液包体、热力学计算(P、T、fo_2、fs_2、pH)的物理化学再造等多学科方法得到的数据表明,以往的剪切模式对准确再现金的来源、富集的作用过程是不适合的。因此,按照现在可得到的定量数据来重新检验这些矿床的各个形成阶段。
The Hercynian zone in Europe controlled several gold mines containing a group of mineralized and some explorable deposits. In the Hercynian stage of late deformation that has an effect on the substrate, many economically valuable gold enrichments are formed. The gold-bearing quartz vein-type mineralization is characterized by multi-stage metallogenesis within the microfractures of mineralization and during the specific phases of fluid drift. Micro-fissures and fluid effects affect the matrix of early-precipitated quartz veins. According to data obtained from multidisciplinary approaches that include tectonic studies ranging from region to microscopic and physicochemical reconstruction of mineral assemblages, fluid inclusions, thermodynamic calculations (P, T, fo_2, fs_2, pH) The exact pattern of re-payment of gold, the role of enrichment process is not suitable. Therefore, the stages of formation of these deposits are re-examined in accordance with the quantitative data now available.