1) Jinqingding gold deposit
金青顶金矿
1.
Jinqingding gold deposit is the biggest single ore vein type deposit in China.
金青顶金矿是我国最大的石英单脉型金矿。
2.
The new data of metallogenic epochs, the zoning of the mineralization , fluid inclusions and deep mining outcrops in the Jinqingding gold deposit have been reviewed comprehensively.
综合评述了金青顶金矿矿化分带、成矿年龄、流体包裹体以及深部采矿露头新资料。
3.
Jinqingding gold deposit is located in the eastern of Jiaodong uplift and in the middle of mineralization zone of Muping-Rushan gold deposit.
金青顶金矿位于胶东隆起东部、牟平—乳山金矿成矿带中部,矿石类型以含金黄铁矿石英脉型为主,矿体以陡倾状产出,矿石垂直分带特征明显,延深大于延长。
2) Jinqingding Gold Deposit
金青顶金矿床
1.
The genesis and concentration regularity of Jinqingding Gold Deposit;
金青顶金矿床成因及富集规律
3) Jinding deposit
金顶矿床
1.
Discovery of Plaeoproterozoic zircon SHRIMP age from Jinding deposit and its geological implications.;
金顶矿床古元古锆石SHRIMP年龄的发现及其地质意义
2.
Jinding deposit is located in the northern part of Lanping basin, western Yunnan Province.
利用澳大利亚Surpac公司的三维立体制作软件将“金顶铅锌矿详细勘探地质报告”中的318个钻孔、14多万个数据和49张勘探线剖面图等资料,首次做出了可从任意角度观察的金顶矿床矿体三维空间实体模型。
3.
Jinding deposit is a famous giant lead-zinc deposit,located in Lanping,Yunnan province.
位于云南省兰坪县的金顶矿床为一世界著名的超大型铅锌矿。
4) Qingshan gold deposit
青山金矿
1.
Qingshan gold deposit occurred in the hydrothermal basin margin which between the Shangdan suture zone and Mianlue suture zone.
青山金矿床位于商丹缝合带及勉略缝合带之间的旬阳热水盆地边缘,矿体呈脉状、囊状、透镜状、似层状等产出,主要位于上泥盆统九里坪组黑色碳质板岩与下石炭统界河街组碳酸盐岩的接触带中。
2.
Based on the geological setting of the deposit genesis and the features of Qingshan gold deposit in Shaanxi,we studied the ore-prospecting targets in the deep and peripheral area of Qingshan gold deposit,ore control factors,statistical law of the ore-forming elements\'s basic analysis,typomorphic features of the pyrite,ore-forming fluids characteristics and the metallogenetic model.
在总结陕西青山金矿床产出地质背景、矿床地质特征的基础上,分析和研究了矿区控矿因素、成矿元素基本分析统计规律、黄铁矿标型特征、成矿流体特征和矿床成矿模式,矿体主要受含矿岩系、岩相和次级构造的控制,从地表到深部金和铁的品位的变化趋势是越来越高,黄铁矿晶体形态以五角十二面体和五角十二面体与立方体聚型为主,流体包裹体为单相及气液两相,均一温度、盐度在垂向上呈正弦波状变化,建立了青山金矿热泉型成矿模式。
3.
It is suggested that Qingshan gold deposit of hot spring type is formed by the chronically repeated recycling,transformation,enrichment and settlement of the Au from the source bed in the Devonian system by the underground hot brine originating from rainfall.
对青山金矿床的野外地质调查以及矿石与围岩的地球化学分析表明,成矿元素以Au-Ag-As-Sb-Ba组合为特征;赋矿地层中Au含量远大于背景值;围岩及矿石都具有较高的U/Th值,其稀土元素配分形式基本一致,且存在Ce负异常和Eu的正异常;成矿流体氢氧同位素值具明显的"氧漂移"现象;成矿流体温度介于160～220℃;流体包裹体中Ca2+,CO2和HCO3-含量较高,显示成矿流体为重碳酸盐-氯化钠型地下热卤水。
5) Jinding Pb-Zn deposit
金顶铅锌矿
1.
Leaching experiments on cadmium release from Cd-rich oxidized rocks at Jinding Pb-Zn deposit;
金顶铅锌矿区铅锌氧化矿石中镉的风化淋滤实验
2.
REE and microthermometric analyses of fluid inclusions in the Jinding Pb-Zn deposit show that homogenization temperature of ore-forming fluid is at 54℃~309℃ and 143℃ in average,and its salinity(ω(NaCl)) is at 1.
金顶铅锌矿床流体包裹体的显微测温和流体的稀土元素特征表明:金顶矿区成矿流体均一温度为54℃~309℃,平均143℃,盐度(ω(NaCl),下文同)为1。
3.
The Jinding Pb-Zn deposit in Yunnan is rich in cadmium,and mining activity facilitates releasing of cadmium into the aquatic ecosystem.
云南金顶铅锌矿是镉(Cd)元素富集区,采矿活动导致Cd释放出来进入地表环境造成Cd污染。
6) Dongfengding gold deposit
东峰顶金矿
1.
The Dongfengding gold deposit is controlled by faulted zones.
东峰顶金矿受断裂破碎带控制，矿石中主要矿物成分有石英、黄铁矿、重晶石及褐铁矿，其标型特征具成因和找矿意义。
补充资料：青顶山
青顶山，海拔239.5米，幅员面积450公顷。山上森林覆盖完好，山峰陡峭，树种较多，风光秀美，环境怡人。有两座庙宇，有神树、狐仙洞、石三坑等自然景观。有凉亭、炮台、疗养院、美食城、雕塑、了望塔等基础设施和旅游景点。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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