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索尔库都克-哈腊苏铜钼金多金属矿集区成矿规律
THE METALLOGENETIC RULE OF SUOERKUDUKE-HALASU CU-MO MULTIMETALLIC CONCENTRATION AREA
【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。
【Abstract】 In this paper,we have summarized the basic characteristics of different ore and genesis type deposits,studied the metallogenetic rule of them in the concentration area.We think the metallogenesis is concentrated 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,Kalatongke Cu-Ni deposit,Suoerkuduke Cu-Mo deposit,with characteristics in zonation distribution,separate concentration,strata,structure,ore control of rock body,tension metallogenesis.
【Key words】 Multimetallic Deposit; Multifactor Ore Control; Multirange Zonation; East Aertai; Xinjiang;
- 【文献出处】 云南地质 ,Yunnan Geology , 编辑部邮箱 ,2011年03期
- 【分类号】P618.41
- 【被引频次】7
- 【下载频次】210