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The hydrothermal gold mineralization occurred in early Yanshanian Period, although the Shuiquangou syenite complex emplaced in Hercynian Period.

矿体具有明显的分层性,自上而下矿石类型由石英脉型向钾、硅化蚀变岩型过渡。

Sylvanite was formed at the late mineralization stage of the Beiling gold deposit and occurs in comby network quartz, associated with native gold.

针碲银金矿产于北岭金矿的晚期矿化阶段,赋存于梳状排列网脉状的石英中,与自然金伴生。

And a few stacks are evidently curved, which shows the compression parallel to the bedding. According to the relation-ship between stack, bedding and hydraulic fractured-filled quartz veinlet, the very low metamorphism is regarded as the product before the regional deformation structure-thermal event.

根据堆垛集合体、层理及早世代水力破裂充填石英微细脉体间关系,认为极低级变质作用是区域变形构造热事件之前的产物:变质温度在 15 5~ 35 0°C之间,变质级、地层时代及岩层在地层柱中的位置渐趋一致,与区域变形强度缺乏谐调关系。

The circulation of volcanic hot spring formed the alteration zone which, together with atmospheric water and subvolcanic hydrothermal solution, formed micro-crystalline quartz that contained adular and sericite.

火山热泉循环形成蚀变晕,此阶段有大气降水的参与;潜火山热液成矿阶段发育的低温微细石英网脉中含冰长石和绢云母。

The geochemical characteristics of REE in the auriferous quartz vein s indicate that the ore forming f.

含金石英脉的稀土元素地球化学特征表明成矿流体具有多源性。

The SiO2 released from fluid-rock interactions occurred in the form of colloid, absorbed gold in the fluids, and then recrystallized to form auriferous quartz veins in the brittle structure.

释放出的SiO2呈胶体态赋存在流体中,并吸附Au等成矿物质,后在脆性构造中重结晶为含金石英脉。

Arsenopyrite, pyrite, chalcopyrite, marcasite, pyrrhotite, sphalerite, galena and boulangerite are the main metal minerals, while the gangue minerals are dominated by quartz, fluorite and calcite.

在野外调研基础上,对主要脉石矿物石英、萤石中流体包裹体进行了包裹体岩相学、显微测温分析和包裹体中气液相成分的LRM分析。

Based on the proven gold deposits, there are three ore-forming types: skarn, altered cataclastic rock and quartz veins.

在已探明的金矿床中,有矽卡岩型、破碎蚀变岩型、石英脉型三类。

Gold ore bodies occur in cataclastic zone.The gold deposits are of complexed mesothermal quartz vein-altered rock type.

金矿体产于断裂破碎带中,为中低温热液石英脉-蚀变岩复合型金矿床。

The fluid inclusion petrography and homogenization temperature of quartz vein type Au ore and the altered cataclastic rock type Au ore (area 210) show different characteristics of the fluid inclusions and variation of the ore-forming temperatures. The fluid inclusions can be divided into Ⅰ and Ⅱ types, i.

通过对北山地区金窝子矿区石英脉型金矿和210矿区蚀变岩型金矿中流体包裹体的岩相学和显微测温研究,查明了不同金矿类型中流体包裹体的特征和成矿温度的变化特征。

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