四川力马河镍矿是峨眉山大火成岩省一个重要的岩浆硫化物矿床。
The Limahe Nickel Deposit is a typical PGE-poor Ni-Cu deposit in the Emeishan Large Igneous Province.
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.
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.
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.
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.
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.
本文简单介绍了该矿床的地质情况，探讨了矿床成因，并在此基础上提出了新的找矿方向：寻找岩浆通道型块状硫化物矿床。
This paper introduces the geology of the deposit, discusses the genesis, and on the basis of these to find a new direction for prospecting : Magma massive sulfide deposit.
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.
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.
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