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1)  massive sulfide Cu-Zn deposit
块状硫化物铜锌矿床
2)  VMS lead and zinc deposit
块状硫化物型铅锌矿床
3)  massive sulfide deposit s
块状硫化物铜矿床
4)  massive sulfide deposits
块状硫化物矿床
1.
Au-bearing Cu-S-Fe massive sulfide deposits at the Tongling mineralized region are characterized by a geological-geochemical "two-member texture".
铜陵矿集区含金铜-硫-铁块状硫化物矿床,具有明显的地质地球化学二元结构性。
2.
The study on modern sea-floor metallic sulfide deposits promoted and advanced the theory on genesis of ancient massive sulfide deposits.
对现代海底金属硫化物成矿作用的研究大大推动和促进了对古代块状硫化物矿床成因的认识。
5)  massive sulfide deposit
块状硫化物矿床
1.
, Hercynian synsedimentary Sedex-type massive sulfide deposits and Yanshanian magmatic deposits.
该区海西期同生沉积的SEDEX型块状硫化物矿床和燕山期岩浆热液矿床的成矿物质来源具有二元性。
2.
The author has collected the data on host rock formations of some well_known volcanogenic massive sulfide deposits and belts both in China and abroad, which include rock associations, time and successions of host rock formations, and rock associations, chem.
双峰式火山岩不仅是火山成因块状硫化物矿床中最常见的含矿岩石组合 ,而且也是研究其古成矿地质背景和成矿作用的主要依据之一。
3.
Research on massive sulfide deposits in the past ten years has made great much advances in deposit classification, mineralization and alteration features, ore textures and structures, ore deformation and metamorphism, deposit models and formation mechanisms, sources of metals and sulfur, properties and sources of mineralizing fluids, and mineralizations on modern seafloors.
最近十余年来,海底块状硫化物矿床的研究在如下方面有新的进展:矿床类型、矿化和蚀变特征、矿石结构-构造和变形-变质、矿床模式和成矿机制、金属和硫的来源、成矿流体的性质和来源,以及现代海盆地中的成矿作用等。
6)  massive sulphide deposit
块状硫化物矿床
1.
There are more than 20 massive sulphide deposits within upper Paleozoic basins inSouth China.
华南海西—印支断裂拗陷带中的块状硫化物矿床(MSD)主要产于晚古生代海侵岩系底部附近碎屑岩向碳酸盐地层的过渡部位,含矿岩系中伴有少量双峰式火山岩和大量喷流岩,矿床中最基本的矿物共生关系是变质反应关系,金属元素和矿物相的分布往往显示地层学垂直分带和侧向分带,这种分带是同生沉积-成岩、活化转移和后期改造叠加等因素综合作用的产物。
2.
Detailed field and laboratory investigations re-vealed that these stratabound orebodies are massive sulphide deposit.
冬瓜山铜金矿床经历了两次成矿作用:第一成矿阶段,在石炭纪中期,海底喷流作用形成了块状硫化物矿床,矿石成分以疏、铁矿为主;第二成矿阶段,燕山期岩浆侵入,一方面岩浆热液与围岩相互作用发生矽卡岩化、硅化、钾长石化、石英绢云母化和青磐岩化,形成矽卡岩型和斑岩型矿体,另一方面岩浆流体对块状硫化物矿体进行叠加改造,致使块状硫化物矿体富集铜等成矿物质。
补充资料:掺杂铜和氯的硫化锌镉
CAS:68512-49-2
中文名称:掺杂铜和氯的硫化锌镉

英文名称:Cadmium zinc sulfide, copper and chlorine doped

cadmium zinc sulfide ((cd,zn)s), copper chloride-doped

Cadmium zinc sulfide,copper and chlorine doped
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