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1)  leadzinc hydrothermal deposit
铅锌热液矿床
2)  volcanogene hydrothermal ore deposit
火山热液型铅锌矿床
1.
In ore-hosting wall rocks,late stage vein rocks and altered rocks of volcanogene hydrothermal ore deposits,the contents of ore-forming elements Pb,Zn and Ag are high,the element associations of ore bodies are complex,the primary anomalies are very developed,and there exists primary zoning.
火山热液型铅锌矿床赋矿围岩、后期脉岩和蚀变岩石中成矿元素铅锌银含量高,矿体元素组合复杂,原生异常发育,并存在着原生分带现象。
3)  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
4)  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
5)  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。
6)  Pb-Zn ore deposit
铅锌矿床
1.
Geological characteristics of Tianshengguan Pb-Zn ore deposit;
天生关铅锌矿床地质特征
2.
With study on the geological settings, ore-forming conditions, deposit geology and tectono-geochemistry of Hetaoping Pb-Zn ore deposit, some acknowledgements have been attained as following: (1) Structures, strata and rocks are the ore-controlling factors;O.
本论文是导师韩润生研究员与薛传东副教授承担的云南祥云县飞龙股份公司项目《保山核桃坪铅锌矿床隐伏矿预测》等项目的资助下顺利完成的。
3.
Polygenetic compound mineralization of Fankou Pb-Zn ore deposit, Guangdong;
认为凡口铅锌矿床属于典型的多因复成矿床。
补充资料:海底热液矿床
海底热液矿床
submarine hydrothermal deposits
    同海底热泉有关的多金属硫化物矿床  。海底热泉自海底喷口喷出。发生于海洋脊轴附近。1965年在红海首次发现。1977年伍兹霍尔海洋研究所R.巴拉德等乘阿尔文号潜水器在加拉帕戈斯裂谷发现的热泉及1977年在北纬21°的东太平洋海隆观察到温度最高达380±30℃的热泉,其热液刚喷出时清澈透明,与海水相混时遇冷便激起混浊的碱性水柱,并析出很细小的铁、铜、锌等的硫化物颗粒,它们堆积在热泉口旁,成为海底热液矿床。矿床类型已发现的超过11处,依产出位置可分为:大洋中脊型、岛弧-边缘海型、热点型和活动断裂型。
    东太平洋海隆热液矿床 属大洋中脊型。以北纬21°处的为例:热泉分布在长仅7千米、宽不过200~300米的狭长条带内,喷口多达25个;各高温喷口周围有块状的金属硫化物堆积,高1~5米,状如黑烟囱,这些沉淀物主要是磁黄铁矿,夹杂着黄铁矿、闪锌矿和铜铁的硫化物;喷口附近水样中He和He的总含量甚高,表明有来自地幔的物质。
    红海热液矿床 以阿特兰蒂斯-Ⅱ号深渊为例:底部为软泥覆盖层,由砖红色软泥与白色、黑色、绿色的薄层相间;主要矿物为细粒的铁蒙脱石、针铁矿、水锰矿、锰菱铁矿及多种金属的硫化物;矿床规模很大,估计锌储量可达320万吨,铜80万吨,铅8万吨,银4500吨,金45吨。
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