摘要
那拉提成矿带地处那拉提-红柳河缝合带,成矿条件有利.通过对铜、金、钨、铁等主要矿种成矿类型的典型矿床分析,认为基底断裂、地壳浅部断裂、岩浆活动、地层等因素是主要的控矿地质因素,从大地构造环境及演化与成矿的关系等方面总结了成矿规律.
Nalati mineralization belt is located at Nalati-Hongliuhe suture belt where mineralizing condition is favorable. Based on the analysis of some typical mineral deposits such as copper, gold, tungsten and iron deposits, it is thought that the main ore-controlling factors are basement fractures,shallow crust fracture, magmatic activity, stratigraphy and geochemistry. Mineralization regularity in Nalati mineralization belt is discussed by the relationship between tectonic settings and evolution with mineralization. Therefore,it is considered that there is great potential of discovering polymetallic ore body in Nalati mineralization belt.
出处
《新疆地质》
CAS
CSCD
2007年第3期253-257,共5页
Xinjiang Geology
基金
新疆西天山那拉提成矿带铜金矿资源潜力评价项目(200410200015)资助
关键词
那拉提成矿带
铜金钨矿
矿床类型
成矿规律
Nalati mineralization belt
copper-gold-tungsten deposits
deposit type
mineralization regularity
