摘要
总结矿集区不同矿种、不同成因类型矿床的基本特征,研究矿床成矿规律,认为成矿集中在海西期,矿床形成先后顺序从早到晚为依次为:乔夏哈拉铁铜金矿、哈腊苏铜金(钼)矿、希勒库都克铜钼矿、沙尔布拉克金矿、喀拉通克铜镍矿、索尔库都克铜钼矿。且具有成带分布、分段集中,地层、构造、岩体控矿,张裂成矿的特点。
In this paper, we have summarized the basic characteristics of different ore and genesis type de- posits, studied the metallogenetic rule of them in the concentration area. We think the metallogenesis is concen- trated in Variscan. The successive formation series early and late of ore deposit is as follows： Qiaoxiahala Fe - Cu - Au deposit, Halasu Cu - Au （Mo） deposit, Xilekuduke Cu - Mo deposit, Shaerbulake Au deposit, Kala- tongke Cu - Ni deposit, Suoerkuduke Cu - Mo deposit, with characteristics in zonation distribution, separate con- centration, strata, structure, ore control of rock body, tension metallogenesis.
出处
《云南地质》
2011年第3期381-385,328,共6页
Yunnan Geology
基金
国家"十一五"科技支撑计划项目-阿尔泰成矿带整体研究与勘查技术集成(项目编号:2007BAB25B01)
关键词
多金属矿
矿集区
多因素控矿
成带多段
新疆阿尔泰东段
Multimetallic Deposit
Multifactor Ore Control
Multirange Zonation
East Aertai
Xinjiang
