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1)  Luojiahe copper deposit
落家河铜矿床
1.
Luojiahe copper deposit in Zhongtiaoshan region is of high grade and median size.
中条山落家河铜矿床处于中元古界西阳河群安山岩复盖区的断裂-剥蚀构造天窗之中,出露了晚太古界绛县群宋家山组一套火山-(喷流)沉积岩建造。
2)  Luju copper deposit
郝家河铜矿
1.
The sandstone-type Cu deposits in th e Chuxiong basin occur in the Cretaceous Gaofengsi Formation and Maotoushan Formation and these o re deposits are represented by the Luju copper deposit and Haojiahe copper deposit.
不论是硫同位素,还是氢氧同位素、铅同位素,六苴铜矿床和郝家河铜矿床均不相同。
3)  Xujiagou copper deposit
徐家沟铜矿床
1.
Xujiagou copper deposit lies in the northwest of Tongchang ore field in the central Mianxian-Lueyang-Yangpingguan copper polymetallic mineralization-intensive area.
徐家沟铜矿床位于勉(县)-略(阳)-阳(平关)铜多金属矿化集中区中部的铜厂矿田西北部,矿体产于中上元古界郭家沟组中的片理化细碧岩带內,已圈定铜矿体13条,多为盲矿体。
4)  Pangjiahe gold deposit
庞家河金矿床
1.
On the basis of an analysis and study on numerous first-hand data from the laboratory and the field,it is preliminarily considered that Pangjiahe gold deposit genetically belongs to mesothermal-epithermal one which resulted from sedimentary-hydrothermal reworking.
根据大量的室内外第一性资料的分析研究,初步认为庞家河金矿床的成因类型属沉积-热液改造型中低温热液矿床,并且揭示了矿床的成矿规律,提出了有关地层、岩性、构造、蚀变以及前缘指示元素等方面的找矿标志,为寻找该类型金矿提供了理论依据。
5)  Niujiaxiaohe gold deposit
牛家小河金矿床
6)  channel throw
河床落差
补充资料:落铜
1.犹落钞。铜;铜钱。
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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