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1)  saline lake deposit
盐湖矿床
2)  lake area deposit
湖域矿床
1.
In the process of large scale mining activities on the lake area deposit, water disasters like surface water spill-in, sudden undergroud water breakout, floor collapse, large area landslide and mudflow,etc.
在分析湖泊形成过程的基础上,将湖域矿床的水文地质特征归为4类:管道涌水类、岩溶滞水类、渗流含水类和无水类。
3)  saline-mineral
盐湖矿产
4)  Dahu gold deposit
大湖金矿床
1.
Discussion of vertical zoning regularity of gold mineralization in the east part of Xiaoqinling area——based on the analysis of Dahu gold deposit;
小秦岭东段金矿化的垂向分带规律探讨——以大湖金矿床为例
2.
In this paper, we choosethe Dahu gold deposit located in the north part of Xiaoqingling area as the target.
论文以小秦岭北矿带大湖金矿床为研究对象,运用流体包裹体岩相学,流体包裹体温度测试,流体包裹体成分分析,氢氧同位素组成测试等方法,讨论了大湖金矿床成矿流体的特征,成矿流体的来源和成矿机理。
5)  Shihu Gold Deposit
石湖金矿床
1.
Based on mine geology and geochemical characteristics of ore trace elements,rare earth elements and stable isotopes in the Shihu gold deposit,the authors have reached the conclusion that the gold ore-bearing horizon is Tuanpokou Formation of Archean Fuping Group.
文章根据冀西石湖金矿床的矿区地质特征、矿石的微量元素地球化学特征、稀土元素的地球化学特征、稳定同位素地球化学特征等的研究,认为金矿赋矿层位为阜平群团泊口组。
2.
Based on mine geology,ore trace elements geochemistry,rare earth elements geochemistry and stable isotopes in the Shihu gold deposit,it is concluded that gold ore-bearing horizon is Tuanpokou Formation of Archean Fuping Group.
通过冀西石湖金矿床的矿区地质特征、矿石的微量元素地球化学特征、稀土元素的地球化学特征、稳定同位素地球化学特征等研究,认为石湖金矿的赋矿层位为阜平群团泊口组,硫、铅来源于地幔,金矿床成矿物质主要来源于矿源层。
6)  rock salt deposit
岩盐矿床
1.
Through analysis on wide application of horizontally butted well in exploiting rock salt deposit and in combination with current situation and existing problems in rock salt mine exploiting in Penglai,this paper forecasts the application prospect of horizontally butted well in exploitation in the future.
通过对水平对接井技术在开采岩盐矿床的广泛应用的分析,结合蓬莱岩盐矿山开发现状及存在的问题,展望了该矿山在今后的开发中,水平对接井技术的应用前景。
补充资料:盐湖
指湖水中含盐度很高的咸水湖。分布在干旱地区。如中国青海的察尔汗盐湖、茶卡盐湖等。当湖中盐分达到饱和状态后,即沉淀为岩盐。
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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