铜镍硫化物矿床是典型的岩浆矿床。
喀拉通克铜镍硫化物矿床是产于我国北疆喀拉通克成矿带内的大型岩浆铜镍硫化物矿床。
The Karatungk magmatic Cu-Ni sulfide deposit exists in the Karatungk metallogenic belt in northern Xinjiang in China.
从赋矿岩体、控矿因素、成矿作用和矿体类型等方面综述了铜镍硫化物矿床的最新研究进展和成果。
The study development of Cu-Ni sulfide deposit is discussed according to the ore-bearing rock-bodies, ore-controlling factors, mineralization and deposit types.
与超基性岩浆作用有关的铜镍硫化物矿床主要有两种成矿建造，一种为含铬建造，另一种为含铂建造。
There are two metallogenic formations for copper nickel deposits related to ultrabasic magmatism, namely chrome and platinum bearing formations.
而与赋存超大型镍铜硫化物矿床的金川岩体相比，煎茶岭超基性岩体为岩浆一次侵位形成，分异程度小，镍、硫含量较低。
However, compared with jinchuan ore - bearing intrusion, jianchaling ultrabasic intrusion formed by magma simple emplacement, and magma fractionated weakly with lower content of nickel and sulphur.
经过大量资料收集、数据整理和建库，完成了中国镍铜铂族岩浆硫化物矿床矿产地数据库的建设。
Through collecting related material, arranging the data and devising the database, the mineral geology database of Chinese Ni-Cu (PGE) sulfide deposit is set up.
中国镍铜铂族岩浆硫化物矿床矿产资源方面，全国尚无统一的矿产地质数据库。
There is no uniform mineral geology database of Ni-Cu (PGE) sulfide deposit in China.
我国的情况更为突出，镍金属储量近86%、铂90%以上、铜约7.3%均来源于铜镍硫化物岩浆矿床。
In China, it is more prominent, about 86% amount of nickel, 90% amount of platinum metals, 7.3% copper comes from nickel-copper sulfide magmatic deposits.
我国的情况更为突出，镍金属储量近86%、铂90%以上、铜约7.3%均来源于铜镍硫化物岩浆矿床。
In China, it is more prominent, about 86% amount of nickel, 90% amount of platinum metals, 7.3% copper comes from nickel-copper sulfide magmatic deposits.
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