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1)  lead_zinc deposit
铅锌黄铁矿-硫锰矿矿床
2)  Pyrite-lead-zinc deposit
黄铁铅锌矿床
3)  zinc-pyrite dpeosit
锌、硫铁矿矿床
1.
The Gaobanhe ore deposit is a well-known zinc-pyrite dpeosit on the northern margin of the North China platform and within the Yanliao metallogenic belt,and the host rocks are sedimentary rocks of Proterozoic Gaoyuzhuang Formation,consisting of manganiferous dolomite,carbonaceous dolomite,siliceous dolomite,siliceous mudstone,manganiferous carbonaceous shale and siliceous banded dolomite.
冀东高板河锌、硫铁矿矿床容矿岩石具有热水沉积岩的地球化学特点。
4)  lead-zinc deposit
铅锌矿床
1.
Identification and study of stockwork altered pipe of Xitieshan lead-zinc deposit,Qinghai Province;
锡铁山铅锌矿床网脉状蚀变管道相的识别与研究
2.
MORPAS-based multi-information prognosis of lead-zinc deposits in Lintan-Dangchang area, Gansu Province;
MORPAS支持下的甘肃临潭—宕昌地区铅锌矿床多源信息预测
3.
Geological-geochemical characters and genesis of the Heshuxia lead-zinc deposit, Guangdong Province;
广东荷树下铅锌矿床地质地球化学特征与矿床成因
5)  Pb-Zn deposit
铅锌矿床
1.
Geological characteristics of the Tonglushang Pb-Zn deposit with its prospecting direction,Northwestern Guizhou;
黔西北地区铜炉上铅锌矿床地质特征及找矿方向
2.
Mineralization characteristics and ore-forming mechanism of the Jianbidong Pb-Zn deposit in Fengshun County,Eastern Guangdong;
粤东丰顺县尖笔岽铅锌矿床矿化特征及形成机理
3.
Geological characteristics and genesis of the Weibao Pb-Zn deposit in Ruoqiang County,Xinjiang;
新疆若羌县维宝铅锌矿床地质特征及成因分析
6)  lead-zinc deposit
铅-锌矿床
1.
The paper summarized the geological cognition of the fomer reseachers on the ore-controlling structure,orebody occurrence characteristics and deep part ore prospecting perspective of the Maomaochang-Zhazichang lead-zinc deposit in Northwestern Guizhou.
阐述了前人对黔西北猫猫厂-榨子厂铅-锌矿床的控矿构造、矿体产出特征及深部找矿前景的地质认识。
2.
Skarn and mesothermal-epithermal fluid filled lead-zinc deposits were found outside the molybdenum deposit during recent years' survey of land and resources,which occur in ring belt surrounding the Nannihu molybdenum deposit.
豫西南泥湖地区具有闻名于世界的特大型钼矿,通过近几年国土资源大调查工作,在南泥湖钼矿外围发现了矽卡岩型和中低温热液充填型铅-锌矿床,它们成环带状分布于南泥湖钼矿外围。
补充资料:锌黄
分子式:
分子量:
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性质:见锌铬黄。

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