通过成矿地质条件分析，内蒙古自治区科尔沁右翼前旗刘店沟矿床的形成与晚侏罗世陆相中酸性火山岩及早白垩世黑云母花岗闪长斑岩、黄铁矿化花岗闪长斑岩关系十分密切，北东、北西向构造为区内主要的控矿构造，北东向构造为导矿构造、北西向构造为容矿构造，因此，地层、岩浆岩、构造“三位一体”控矿为本区控矿规律。成矿时代为早白垩世晚期。成因类型为岩浆热液型。

Through the analysis of metallogenetic geological conditions, the formation of Liudiangou silver deposit in Horqin Right Front Banner of the Inner Mongolia related to the Late Jurassic continental facies intermediate acidity volcanic rock and the Early Cretaceous biotitic granodiorite porphyry, pyritized granodiorite porphyry. The NE, NW direction structures are the main ore-control structures in the region, the former is ore-bringing structure, the latter is host structure, therefore, strata, magmatic rocks, structures of“the Trinity”ore-controlling are ore-control regularity in this area. The metallogentic epoch is the late stage of the Early Cretaceous. Genetic type is a magmatic hydrothermal type.

该作者结合深部找矿实践及地球物理测量成果，提出矿区存在重要的控矿隆起构造的观点，通过分析总结隆起构造的控矿特征，指出了矿区外围及其深边部找矿有利地段，指导矿山企业深部找矿探矿工作。

Based on practice and geophysical survey results of the deep prospecting, mining area is the important ore-control ing arched structure is put forward, analysis summary ore-control ing characteristics of arched structure, points out the favorable mining area peripheral and depth of prospecting and mining enterprises of deep ore prospecting work.

内蒙古常福龙金矿床位于华北地台北缘中段区域EW向韧性断裂的次级NWW剪切带系统内。金成矿发生在燕山晚期，处于区域构造体制挤压－伸展－挤压的转换期以及2期近南北向大规模构造推覆作用的间歇期，张性构造环境为剪切带流体汇聚与成矿作用创造了条件。剪切带构造控矿主要表现为主断裂构造透镜体控矿、主断裂局部张性部位控矿和次级张性断裂－裂隙控矿3种基本型式，构造－流体共同作用分别形成了蚀变岩型、角砾岩型和石英脉型矿化（体），形成了常福龙剪切带型金矿床构造－蚀变网络基本格局。可以考虑利用构造－蚀变网络结构上的自相似性，指导矿山深边部找矿勘查以及剪切带系统内新矿体的预测。

Changfulong Gold Deposit in Inner Mongolia is hosted in the secondary NWW trending shear zone sys -tem of the regional EW trending ductile fault locating at the middle of the north part North China Craton .Gold mineral-ization occurred in Yanshanian .It is a time that regional tectonic regime transited from compression to extension and to compression ,and a period just between the large scale of regional thrusts in this area .Tensile tectonic environment supplied the possible conditions for ore fluids concentration and related mineralization in the shear zone .Ore types in the structural ore-controlling shear zone can be classified into the main fault tectonic lens controlling types ,the main fault local tensile fracture controlling types and the secondary tensile fracture -fissures controlling types .Coupling of structural deformation and fluid flow in the shear zone formed the different ore mineralization of altered rocks type , breccias type and quartz vein type , which es

易门凤山铜矿床是昆阳元古宙裂谷铜矿带易门式铜矿床的典型代表之一。该矿床明显受刺穿体构造控制，铜矿体赋存于昆阳群绿汁江组硅化碎裂白云岩中。根据刺穿体的宏观分布特征、岩石学和岩石地球化学特征，进一步剖析了控矿型刺穿体和非控矿型刺穿体两种类型：控矿型刺穿体岩石成份复杂，构造变形强，角砾状构造发育， MgO含量变化大（3.18%~15.64%）， FeO/Fe2O3值变化范围大（0.43~28.50），其形成机制与深部火山隐爆作用和强烈构造作用有关；而非控矿型刺穿体岩石成份简单，内部构造变形弱，角砾状构造不显著， MgO含量低（1.90%~3.77%）， FeO/Fe2O3值也低（0.14~0.56），其形成机制主要与强烈构造作用有关。建立了控矿与非控矿型两类刺穿体的岩石地球化学特征和识别标志。该标志对该类矿床的找矿预测具有实际意义。

TheYimen Fengshan copper deposit is one of the typical examples of copper deposit in the Kunyang rift basin, Yunnan province, China. The ore-bodies are located in the cataclastic dolomite of the Lvzhijiang Formation which was controlled by diapir structure. This study suggests that not all diapir hosts ore-bodies. Diapir may be divided into the ore-controlling type and non-ore-controlling type. The two types of diapirs have obviously different macro-distribution, petrography, and geochemical characteristics. The rocks from the ore-controlling type diapir have composition and pre-tectonic recrystallization more complex than these of the non-ore-controlling type diapir. Moreover, the rocks in the ore-controlling type diapir are closely related to crypto-explosionsas indicated by the intermediate-acid crystal tuff breccias and dacite breccias. In addition, the geochemical characteristics of rocks from the ore-controlling type diapir have higher MgO contents (3.18% to 15.64%), an

广西凤山县金牙金矿是我国滇黔桂金三角地区具代表性的微细浸染型矿床之一。文章通过地质构造调查，综合分析了矿床构造特征，控矿构造，矿区构造样式等，认为金矿体主要分布在背斜的转折端及东西两翼。矿区断裂构造有近SN向主断裂、近SN向次级断裂、以及顺层滑动破碎带等，它们均为区内控矿构造。其中近SN向次级断裂是主要的容矿构造，通过对其运动学特征研究认为它们为早期挤压过程中派生的X节理，次级断裂后期张扭性活动叠加成矿作用。在此基础上，提出了金牙金矿床的找矿前景。

Jinya gold deposit in Fengshan county of Guangxi Zhuang Autonomous Region is a typical fine disseminated deposit which locates at the triangle region of Yunnan-Guizhou-Guangxi. The comprehensive analysis on structural fea-tures, ore-controlling structure and tectonic style of Jinya gold deposit during the geological structure survey shows that gold ore bodies are distributed in the hinge zone and the east and west limbs of the anticline. The mineralization is controlled by the faulted structures in this mining area, which are nearly SN trending master fault, nearly SN trending subsidiary fault and bedding gliding broken belt. Among them, nearly SN trending subsidiary fault is the major ore-bearing structure, and its kinematics characteristics were researched. In light of the results, these structures are X-joints which occurred in the compressive setting during the early stage. The subsidiary fault is superimposed by tensor-shear activities in some parts, and superimposed mineralizatio