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The Gejiu (个旧) deposit is a superlarge tin-copper polymetallic ore-forming concentration area characterized by excellent metallogenic geological settings and advantageous ore-controlling factors. The deposit displays diverse mineralization properties due to different minerals and mineral deposit types. Based on the principal metallogenic factors, metallogenic mechanisms, mineralized components, and occurrence of mineral deposits or ore bodies, the Gejiu mineral district can be divided into 2 combinations of metallogenic series, 4 metallogenic series, 8 subseries, and 27 mineral deposit types. Spatial zonality is evident. The distribution regularity of the elements in both plane and section is Be-W, Sn (Cu, Mo, Bi, Be)-Sn, Pb, Ag-Pb, Zn around a granitic intrusion. The metallogenic epoch is mainly concentrated in the late Yanshanian. During this period, large-scale metallogenic processes related to movement caused by tectonics and magmatism occurred, and a series of magmatic hydrothermal deposits formed. The ore-forming processes can be divided into 4 stages: the silicate stage, the oxide stage, the sulphide stage, and the carbonate stage. Based on the orderliness and diversity (in terms of time, space, and genesis) of the mineralization, the authors have developed a comprehensive spectrum of ore deposits in the Gejiu area. This newly proposed diversity of mineralization and the spectrum developed in this work are useful not only for interpreting the genesis of the Gejiu deposit but also for improving mineral exploration in the area, and in particular, for finding large deposits. 相似文献
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针对遥感图像融合Brovey变换法存在颜色失真的现象,提出了一种低通比值融合法。该融合方法首先对高几何分辨率的全色波段进行低通滤波,然后将低分辨率多光谱图像与全色波段图像相乘,再除以滤波后的全色波段图像,便得到融合图像。从辐照的角度证明了该低通比值融合法具备理论基础,并从目视评价、定量分析、分类精度证实了该低通比值融合法优于Brovey变换法。该低通比值融合法是一种能较好地保全低分辨率多光谱图像颜色的融合方法。 相似文献
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An Erratum has been published for this article in Earthquake Engineering and Structural Dynamics 2000; 29(7):1076. Two interrelated issues related to the design of non-linear viscous dampers are considered in this paper: structural velocities and equivalent viscous damping. As the effectiveness of non-linear viscous dampers is highly dependent on operating velocities, it is important to have reliable estimates of the true velocity in the device. This should be based on the actual relative structural velocity and not the commonly misused spectral pseudo-velocity. This is because if spectral pseudo-velocities (PSV) are used, they are based on design displacements (Sv=ω0Sd) and are thus fundamentally different from the actual relative structural velocity. This paper examines the difference between these two velocities, and based on an extensive study of historical earthquake motions proposes empirical relations that permit the designer to transform the well-known spectral pseudo-velocity to an actual relative structural velocity for use in design. Non-linear static analysis procedures recommended in current guidelines for the design of structural systems with supplement damping devices are based on converting rate-dependent device properties into equivalent viscous damping properties based on an equivalent energy consumption approach. Owing to the non-linear velocity dependence of supplemental devices, an alternative approach for converting energy dissipation into equivalent viscous damping is advanced in this paper that is based upon power consumption considerations. The concept of a normalized damper capacity (ϵ) is then introduced and a simple design procedure which incorporates power equivalent linear damping based on actual structural velocities is presented. Copyright © 1999 John Wiley & Sons, Ltd. 相似文献
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非线性粘滞阻尼器消能结构减振效果分析 总被引:5,自引:1,他引:4
应用并完善了非线性粘滞阻尼器消能结构地震反应预测的反应谱方法,通过与时程分析计算结果对比证明了方法的可行性。利用本方法研究了支撑刚度及阻尼器参数对非线性粘滞阻尼器减振效果的影响。通过数值分析,给出了位移降低率达到最佳时支撑刚度取值的建议式。提出了为保证剪力降低率不大于1时非线性粘滞阻尼器参数的控制方法。 相似文献
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胶莱盆地南缘沿五莲-青岛深大断裂及其次级断裂,目前已发现大量的金铅锌多金属矿床(点),除典型的隐爆角砾岩型五莲七宝山金铜矿外,其余各矿床沿断裂发育,以石英脉型矿化为主,均显示热液矿床特征。高家宅科地区已发现的金铅锌多金属矿点,分布在以高岭断裂为主的NNW—近SN向断裂中,但基于成矿规律及成矿作用等认识的不足,该地区找矿工作进展缓慢。本次研究通过短波红外光谱测量,在该地区识别出以伊利石、白云母、绿泥石、高岭石、蒙脱石和菱铁矿为主的蚀变矿物,以面积性绢云母蚀变为主(伊利石+白云母)。绢云母矿物高IC值和低Pos2200吸收峰值分布区域均与区内NNW—近SN向断裂和绢英岩化蚀变带具良好的相关性。结合已有成矿事实,认为区内以高岭断裂为主的NNW—近SN向断裂更靠近热液中心,同时,绢英岩化蚀变带中异常的高IC值和极低的Pos2200吸收峰值分布区域,同样具成矿的可能性。 相似文献