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1)  Xiahaoping gold deposit
下蒿坪金矿
2)  Xiasongping in Henan
河南下蒿坪
3)  Daping gold deposit
大坪金矿
1.
Concentration of platinum group elements(PGE) of various gold ores and around rocks and Re-Os isotopic compositions of major ore minerals of Daping gold deposit were analyzed by using an inductively coupled plasma mass spectrometry(ICP-MS) with nickel sulfide fire assay pre-concentration and carius tube decomposing technique with acetone extracted Re method.
采用镍硫火试金ICP-MS法和Carius管溶矿与ICP-MS联合测定法分析了云南大坪金矿各类金矿石和主要围岩的PGE和矿石矿物的Re-Os同位素组成,结果显示各类金矿石的ΣPGE变化较大,为(3。
2.
Mineralization epochs of the Daping gold deposits are divided into three stages:the early stage or scheelite-bearing quartz vein stage,the major stage or massive polymetallic sulphide typed auriferous quartz vein stage and the late stage or carbonate-quartz stage.
大坪金矿成矿可分为三个成矿阶段:早期成矿阶段(白钨矿石英脉)、主成矿阶段(团块状多金属硫化物含金石英脉)和晚成矿阶段(碳酸盐石英脉)。
4)  Dongping Gold Mine
东坪金矿
1.
The application of filling technique of filling-mining method in Dongping Gold Mine;
东坪金矿充填采矿法充填工艺的实践
5)  Dongping gold deposit
东坪金矿
1.
The faults of various times coincided with,and rebuilded by the ore-formation in the later mineralizing process,and became the ore-occurrence structures of the Dongping gold deposit.
运用里德尔 (Riedel)剪切裂隙理论 ,在东坪金矿构造区域内划分出若干种剪切类型。
2.
4 Ma, showing a significant time gap as compared with the ore-forming age of the spatially closely related Dongping gold deposit.
本文对与东坪金矿有密切空间关系的上水泉花岗岩进行了单颗粒锆石U-Pb同位素定年,结果为135。
3.
The natural gold from Dongping gold deposit is various in morphological characteristic,mainly in form of inclusion gold and fissure gold with large grain size (0.
东坪金矿自然金形态多样,主要以包裹金和裂隙金为主。
6)  Jinjiaping manganese deposit
金家坪锰矿
1.
Through analyzing regional geological setting and geological characteristics in Jinjiaping manganese deposit,it is supposed that the formation of manganese deposit in this area is divided into such 4 stages as continental facies,marine facies,solidification-dehydration-crystallization of ore-forming materials,the deposit is classified into marine sedimentation-sub-recomposed deposit.
通过对该区区域地质背景及金家坪锰矿地质特征的分析,认为该锰矿石形成可分为陆相期、海相期、成矿物质固化失水结晶期及成矿后裂隙充填期4个阶段。
补充资料:蒿径
1.指长满杂草的小路。
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