Ore Genesis in Fracture-Controlled Hydrothermal Systems: Percolation Theory Approaches

机译：裂缝控制热液系统中的矿石成因：渗流理论方法

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Coupling between deformation processes and rock permeability is a major factor influencing the architecture of fluid migration and the localisation of ore deposition in several types of hydrothermal ore systems in middle to upper crustal regimes. Permeability in many hydrothermal systems is controlled by a dynamic competition between deformation-induced porposity-creation processes and porosity-destruction processes. Localisation of deformation within faults, fractures and shear zones leads to flow localisation, with large-scale flow systems forming when active faults and shear zones link to create percolation networks.

机译：变形过程与岩石渗透率之间的耦合是影响流体运移体系结构以及中上地壳区几种热液矿石系统中矿石沉积局部化的主要因素。在许多热液系统中，渗透率是由变形诱发的孔隙形成过程与孔隙破坏过程之间的动态竞争控制的。断层，裂缝和剪切带内变形的局部化导致流动局部化，当活动断层和剪切带连接形成渗流网络时，形成大规模流动系统。

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《International Congress on Earth Science, Exploration and Mining Around the Pacific Rim 10 - 13 October 1999 Bali, Indonesia》|1999年|p.639-642|共4页
会议地点 Bali(ID);Bali(ID)
作者
S.F. Cox; M.A. Knackstedt;
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Ore Genesis in Fracture-Controlled Hydrothermal Systems: Percolation Theory Approaches

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