喀拉通克Ⅰ号硫化铜镍矿床地球化学特征及矿化富集规律探讨  

STUDY ON GEOCHEMICAL CHARACTERISTICS AND MINERALIZATION ENRICHMENT REGULARITY OF KARATUNGKE NO. I CU, NI-SULPHIDE DEPOSIT, XINJIANG

作　　者：帕拉提.阿布都卡德尔 

机构地区：[1]新疆工学院地质系

出　　处：《新疆地质》1991年第4期376-382,共7页Xinjiang Geology

摘　　要：喀拉通克I号铜镍矿床是与基性杂岩体有关的岩浆硫化物矿床.矿床∑REE和稀土配分模式与国内同类矿床相似.铜、镍、钴等主要元素和金、银、铂等贵重金属元素赋存规律明显,与矿化富集规律计算机模拟结果吻合.岩石模式年龄等数项测试分析.为矿床的形成(物理化学条件分析)提供了较合理的依据.The karatungke No.I Cu, Ni-sulphide deposit is a magmatic sulphide deposit related to basic complex rocks. Its REE and partition pattern are similar to those of deposits of same type in other regions of china. Main elements such as copper, nickel and cobalt and precious metal elements such as gold, silver and platinum have an obvious enrichment regularity, which coincides with the Computer modelling results. Analysis of modelling ages of rocks as well as analysis of geochronology, thermodynamics and lithogeochemistry provide the basis for the formation of the deposit.

关 键 词：新疆 喀拉通克 硫化铜镍矿床 地化特征 矿化富集规律 

分 类 号：P5[天文地球—地质学]