1) cassiterite-polymetallic deposit
锡石-多金属矿床
2) tin polymetallic deposit
锡多金属矿床
1.
Discovery of diarite at the depth of the Dajing tin polymetallic deposit and its significance for exploration;
大井锡多金属矿床深部闪长岩体的发现及找矿意义
2.
Tin polymetallic deposit in Changpo district are located in west ore zone of Dachang tin polymetallic ore field,which is formed under the integrated function of strata,fractures and magmatic rocks,namely stratum is the basic condition while structure played ore conducting function and the magma provided heat source and possible ore liquid or matter.
长坡区锡多金属矿床位于大厂锡多金属矿田的西矿带,它是在地层、断裂构造和岩浆岩“三位一体”作用下形成的,地层是基础条件,断裂构造起了主导作用,岩浆提供热源以及可能提供了液源甚至矿质。
3) tin-polymetallic deposit
锡多金属矿床
1.
Fluid inclusion studies of Longshang tin-polymetallic deposit in Xitian ore field,eastern Hunan Province;
湘东锡田垄上锡多金属矿床流体包裹体研究
2.
~(40)Ar/~(39)Ar isotopic dating of the Longshang tin-polymetallic deposit, Xitian orefield, eastern Hunan;
湘东锡田垄上锡多金属矿床~(40)Ar/~(39)Ar同位素定年研究
3.
Based on the spatial analytical module of MAPGIS system, this paper tries to carry out the statistical analysis of a large regional spatial data, and statistically analyses some properties of the related objects including favorable ore-forming strata, structure, magmatic rock and the distribution trend of tin-polymetallic deposits in South China.
基于 MAPGIS系统平台空间分析方法的特点 ,以华南地区的锡多金属矿床为空间分析对象 ,对锡多金属矿床的分布态势及有利成矿地层、构造、岩浆岩等要素的相关对象属性进行了统计分析 ,初步总结出华南地区燕山期和晋宁期岩浆岩、泥盆系和侏罗系地层及 NE向或 NEE向断裂带等有利因素的叠加复合部位是寻找锡多金属矿床的有利成矿条件组合标志 ,为成矿预测及相关区域找矿工作的部署提供了量化依
4) copper-tin polymetallic deposit
铜-锡多金属矿床
1.
Geological characteristics of the Dajing copper-tin polymetallic deposit and its genesis;
大井铜-锡多金属矿床地质特征及其成因
5) Sn-Fe polymetallic deposit
锡铁多金属矿床
1.
The exhalative genesis of the stratabound skarn in the Huanggangliang Sn-Fe polymetallic deposit of Inner Mongolia;
内蒙古黄岗梁锡铁多金属矿床层状夕卡岩的喷流沉积成因
6) Deposits of Sn-polymetals
锡-多金属矿床
补充资料：锡石
| 锡石 cassiterite 锡的氧化物矿物。成分为SnO2。含锡78.6％，是常见的锡矿物，炼锡的最主要矿物原料。常含铁、钽和铌等氧化物的细分散包裹物。四方晶系，晶体常呈四方双锥状，双锥短柱状；膝状双晶常见。集合体大多呈粒块状；外壳呈葡萄状等而内具同心放射纤维构造的称木锡石。纯净者几乎无色 ，一般呈黄棕至棕黑色；条痕白色。金刚光泽，断口呈油脂光泽。莫氏硬度6～7，比重6.8～7.1。主要产于花岗岩分布地区的伟晶岩、气化高温热液矿脉中。因其硬度高、比重大、抗风化力强，常富集成砂矿，称砂锡。中国、马来西亚、印度尼西亚、玻利维亚、泰国等是锡石的主要出产国。中国以广西南丹大厂规模最大；云南个旧锡矿开采历史悠久，有锡都之称。
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