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- Gaolong Au deposit is a sedex deposit in Dian-Qian-Gui rift. 高龙金矿为产于滇黔桂裂谷中的热水沉积型矿床。
- Dongchuang Pb Au deposit is a large quartz vein type deposit. 东闯铅、金矿床是一大型石英脉型矿床。
- Yangshan Au deposit is an unexploited giant deposit. 阳山金矿床为一尚未开发的特大型金矿床。
- Paishanlou large size Au deposit is hosted by tonalite in which upper crustal amphibolitic rock inclusions occur. 研究结果表明，排山楼金矿的容矿围岩是一套以英云闪长岩为主体，含少量角闪质上壳岩包体及脉岩的组合。
- The host rocks of Zhaishang Au deposit are mainly argillic, calc and carbonaceous slates and silty sandstone. 摘要寨上金矿区赋矿岩石主要为泥质、钙质、碳质板岩、粉砂岩等。
- Combination of geochemical exploration and geology leads to the discovery of Jinlongshan Au deposit. 摘要金龙山金矿是化探与地质普查相结合的方法找到的。
- The Au deposit of West Java is situated in the Xijiaowan volcanite Au,Pb,Zn,Cu multimetallic metallogenetic zone. 西爪哇金矿位于印度尼西亚西角湾火山岩金、铅锌铜多金属成矿带,该区有众多金矿床(点)。
- In this paper,we think they must be excluded from the "Carlin-type Au deposit" and call them basaltic Au deposit anew. 本文提出应从“卡林型金矿”中剔除,另行命名为玄武岩金矿。
- The deposit is a medium-low temperature altered cataclastic rock type Au deposit. 金矿床属中低温热液构造蚀变岩型金矿。
- Jiuduigou Au deposit is controled by volcanic breccia body and compressional faults. 九对沟金矿床受火山角砾岩体及张扭性断裂带控制;成矿元素在角砾岩体中富集;
- It belongs to the micrograined Au deposit of structural hydrothermal alteration type. 明显受构造、地层及岩性控制,属构造一热液蚀变岩型微粒金矿。
- The host rocks of Zhaishang Au deposit are mainly argillic,calc and carbonaceous slates and silty sandstone. 寨上金矿区赋矿岩石主要为泥质、钙质、碳质板岩、粉砂岩等。
- And the lateritic Au deposit is also influenced by the land form, eluvial-slope wash and weathering crust degvelopment. 红土型金矿还受地形、残坡积层、风化壳发育程度影响。
- The discovery of large scale Tuobuka Au deposit shows the Au-prospecting potentiality in Dongchuan region. 超大型拖布卡金矿的发现,表明东川地区具备找金前景。
- The Jingushan Au deposit occurred in the Kedao Formation strata,the mineralizing type belongs to structural altered rock one. 金谷山金矿床产于上古生界二叠系柯岛组地层中,矿化类型为构造蚀变岩型。
- The Houdidong Au deposit occurred in the Permian, Kedao Formation contact zone between metamorphic rock series and Variscan gabbro body. 后底洞金矿床产于二叠纪柯岛组变质岩系与华力西期辉长岩体内外接触带。
- The Malutang Au deposit is controlled by NW-trending fractures with Au mineralization associated with pyritization,arsenopyrite mineralization and silicification. 马鹿塘金矿床主要受北西向断层控制,与金矿化有关的蚀变主要为黄铁矿化、毒砂矿化、硅化等。
- Xialiangzi Au deposit is a stratobound Carlin-like type characterized by superimposition and rework of sedimentation, magmatism and brittle ductile shearing. 摘要下梁子金矿床为叠加改造式层控类卡林型金矿床，集沉积地层、岩浆活动、脆韧性剪切构造活动三位一体；
- In this paper,we summarize systematically the metallizing characteristics,metallogenetic rule of the Xiaoshuijing Au deposit and prognosticate the goo... 文中系统介绍小水井金矿矿化特征和成矿规律,进行区域地层、构造、化探异常综合分析,预测该区(外围)较好的找矿远景。
- The Baoxingchang Au deposit lies in the west Yunnan alkaline porphyry Au-Cu-polymetallic metallogenic belt.It is a typical structurealtered rock type Au deposit. 宝兴厂金矿床位于滇西碱性斑岩金、铜多金属成矿带南部,是典型的构造蚀变岩型金矿床。
