金矿

The Correspondence Analysis Method and a successful example of its application for extraction the auriferous alteration zones in the Hadamengou gold ore deposit have been presented in the paper.

介绍了对应分析方法及其在成功提取哈达门沟金矿含金蚀变岩带信息的应用实例。

To reveal the features of axial element zoning of gold deposits in the Chifeng-Chaoyang auriferous province,zonal sequence for 9 gold deposits in the province have been summarized.

为了研究赤峰-朝阳金矿化集中区内金矿床的元素轴向分带特征，归纳总结了区内9个矿床的分带序列。

This paper introduced backwall grouting process and grouting effect of-290 level downcast shaft in Jilongshan Gold Mine.

介绍了湖北鸡笼山金矿-290中段进风井壁后注浆施工工艺过程和注浆效果，并对壁后注浆技术经济效益进行了分析。

The gold ore types are mainly cataclastic and altered rock type.

红土沟-川刺沟金矿是一种典型的造山带中的韧性剪切带型金矿床，其主要的矿石类型为构造破碎蚀变岩型金矿石。

The Wendeng gold deposit is a tectonic breccia cataclastic rock type gold deposit dominated by brittle shear zone and formed by brittle shearing.

文登金矿是受脆性剪切带控制的构造角砾岩碎裂岩型金矿床，是脆性剪切作用形成的，为典型的动力成岩成矿。

Gold mineralization is controlled by the near E-W-trending fault. The metallogenesis belongs to cataclastic altered rock type, with characteristics of low grade and large amount of ore, which is the first discovery in western Liaoning.

通过钻探证实，金矿化受近东西向断裂构造控制，矿化类型为碎裂蚀变岩型，具有低品位、大矿量特点，在辽西地区属首次发现。

Along with the mining industry declining, the settlement distribution, the population aging (in 96 year Tongshan Village old person ratio nearly 30%) with industrial reforming, under such environmental chane, Japanese Colonial Periodaround the time, the gold ore prosperous time, after the Recession of Taiwan in the recovering time historical vein, the substantive space, how does the social space's change live regarding the place maintains with is balanced; How between the reciprocity to achieve settlement old person each other's interaction and the familiar environment?

随著矿业的没落，聚落的分布，人口的老化(96年铜山里老人比率近30%)与产业的转型，在这样的环境变迁下，日治时期前后、金矿兴盛时期、光复时期之后的历史脉络里，实质空间、社会空间的改变对於地方之居住如何相维持与平衡；相互关系之间如何达到聚落老人彼此的互动与熟悉的居住环境？

SOM in Lannigou deposit consisted of coaly organic matter and pyrobitumen.

烂泥沟金矿固体有机质由原生煤系有机质和异源焦沥青组成。

The characteristics of elements shows that magma of fine dioritequartz diorites derived from the enriched mantle or lower crust undergone ocean crust subducting and dehydrating, and was formed and emplaced in the process of crust growth. The magma of dioritic porphyritedacitic porphyries emplaced relatively late, it might derive from upper crust or undergo intensive contamination of crustal materials, and was formed in the proces of crust thining. These characteristics suggest that the geodynamics background of the Jinchanggouliang gold deposit formation is the transition process from compression to extension.

元素地球化学特征显示：细晶闪长岩-石英闪长岩的岩浆源于富集地幔或洋壳俯冲脱水交代的下地壳，地壳增厚过程产生并就位；闪长玢岩-英安斑岩类的岩浆就位相对晚，来源具有上地壳性质或被地壳物质强烈混染，地壳减薄过程形成；这种特征暗示金厂沟梁金矿形成的地球动力学背景是在地壳挤压增厚转化为伸展减薄过程。

The primary ores of the Laozuoshan gold deposit is a heavily disseminated and massive gold ores the main metallic mineral of which is pyrrhotite that account for approximately 11% occurring in migmatitic granite in disseminative and massive form and its gangue minerals take about 80% with quartz and feldspar as main minerals.

老柞山金矿原生矿石为稠密浸染状、致密块状金矿石，矿石中主要金属矿物为磁黄铁矿，约占11%，磁黄铁矿以浸染、致密块状分布于混合花岗岩中；脉石矿物约占80%，以石英、长石为主。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。