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Relationships between deformation and mesothermal veins in the Sunshine Mine Area, Coeur d'Alene district, Idaho

机译:爱达荷州Coeur d'Alene District阳光矿区变形与清热静脉之间的关系

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摘要

The Coeur du27Alene district in northern Idaho is a world class Pb-Ag mesothermal vein system that has produced about 360 million ounces of silver, lead, and zinc since the 1880s. Despite the long history of exploration and production, the district does not have a predictive model for exploration based on a sound understanding of structural controls on the silver ore deposits; this is certainly the case for the Sunshine Mine and surrounding area. Fault kinematic history in the district shows a regional scale fault system reactivated over time with dextral, sinistral, and dip-slip displacement. The fault system is superimposed on regional deformation fabrics that were examined for this study in the Sunshine Mine area. Cleavage sets observed in the Sunshine mine area, distinguished by orientation and superposition relationships, are consistent with the findings of Smith (2004) which defined cleavage sets referred to as S1, S2, and S3. Two additional deformation fabrics that appear spatially tied to fault zones formed between development of cleavages S2 and S3. The multiple cleavages, fault zones, and their intersections are interpreted to act as pathways for hydrothermal fluids associated with vein formation and silver ore deposition. Thin section kinematic analysis of vein and shear zone samples defined a dip-slip sense of shear associated with the Sterling vein. Electron Backscatter Diffraction (EBSD) analysis of vein and shear zone samples failed to define a lattice preferred crystallographic orientation that defined shear sense. Similarly, cathodoluminescence (CL) analysis of thin section textures failed to define a dominant shear sense and fault kinematics. Nevertheless, additional study using these techniques is warranted. Both field observation and thin section analysis demonstrate a direct relationship between shear zones, veins, and mineralization potential, clarifying the need for detailed fault maps for the Sunshine Mine area and Coeur du27Alene district.
机译:Idaho北部的Coeur D U27alene区是世界级的PB-AG Mesothermal静脉系统,自1980年代以来生产了约3.6亿盎司的银,铅和锌。尽管勘探和生产历史悠久,但该区基于对银矿矿床对结构控制的声音理解,该区没有预测模型。这肯定是阳光矿和周边地区的情况。该地区的出现运动历史历史显示区域尺度故障系统随着时间的推移而随着时间的推移,探索和浸渍流离失所。故障系统叠加在阳光矿区在该研究中检查的区域变形织物上。在阳光矿区观察到的裂解组,通过取向和叠加关系的特征,与史密斯(2004)的结果一致,其定义了称为S1,S2和S3的切割集。两种额外的变形织物,其出现在切割S2和S3的显影之间形成的故障区域。多种裂解,断层区域及其交叉点被解释为充当与静脉形成和银矿沉积相关的水热流体的途径。晶段静脉和剪切区样品的运动学分析定义了与英镑静脉相关的剪切浸剪。静脉和剪切区样品的电子反向散射衍射(EBSD)分析未能定义定义剪切感的晶格优选的晶形取向。类似地,阴极发光(CL)对薄剖面纹理的分析未能定义主要的剪切感和故障运动学。然而,有必要使用这些技术的额外研究。田间观察和薄剖面分析展示了剪力区,静脉和矿化潜力之间的直接关系,阐明了阳光矿区和Coeur D U27alene区的详细故障图。

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    Jaclyn Marie Ferraro;

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