1) young miner
矿山的青工
2) 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。
3) The Young Miner
青年矿工
4) Daqingshan gold ore
大青山金矿
5) Qinshan gold deposit
青山金矿床
1.
The Qinshan gold deposit is located at the passive continental margin of Yangzi Plate and belongs to Zhen\'an - Xunyang Strata distict.
青山金矿床大地构造位置属扬子板块被动大陆边缘。
6) Au deposit
青山洞金矿
1.
Discussion on genesis and prospecting model of Au deposit in Qingshandong
青山洞金矿床成因及找矿模型探讨
补充资料：青工
1.青年工人的省称。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条