首页 | 本学科首页   官方微博 | 高级检索  
     检索      

云南格咱岛弧成矿带铜厂沟铜钼多金属矿床地球化学特征及地质意义
引用本文:彦廷龙,刘学龙,李洪宝.云南格咱岛弧成矿带铜厂沟铜钼多金属矿床地球化学特征及地质意义[J].矿产与地质,2016(3):332-337.
作者姓名:彦廷龙  刘学龙  李洪宝
作者单位:1. 昆明理工大学 国土资源工程学院,云南 昆明,650051;2. 通辽市鑫源矿业有限公司,内蒙古 通辽,028000
基金项目:云南省教育厅基金项目“云南格咱岛弧成矿带斑岩型铜矿成矿系统研究“(2015Y066),云南省香格里拉县格咱地区铜多金属矿整装勘查区专项填图与技术应用示范专题二项目(12120114013701)项目;昆明理工大学省级人培项目:云南省香格里拉县铜厂沟斑岩型钼铜矿床成矿系统研究(KKSY201421042),中国博士后科学基金项目(2014M552547XB)联合资助。
摘    要:通过对铜厂沟矿区花岗闪长斑岩地球化学元素及矿区地质特征分析研究,区内的花岗闪长斑岩SiO2含量为66.32%~69.60%,Al2O3含量为14.05%~15.55%,MgO含量为1.19%~1.39%,铝饱和指数A/CNK值为0.88~1.05,属于准铝质-弱过铝质,全碱(K2O+Na2O)含量为6.97%~9.11%,相比中酸性岩石碱度较高。岩石中的轻稀土比较富集(LREE/HREE=13.56~16.94),轻重稀土分馏明显(LaN/YbN=25.97~36.73),δEu(0.87~1.01)、δCe(0.89~0.94)均无明显的异常。富集大离子亲石元素(LILE,Rb、K、La、Ba),相对亏损高场强元素(HFSE,Nb、Hf、Ti),指示岩石是与板块俯冲相关的造山花岗岩系列。矿床中斑岩型矿体与岩浆侵入成矿作用关系密切,而矽卡岩型-热液脉型矿体与岩浆热液上侵充填-接触交代作用相关,矿区深部工程已揭露出深部存在隐伏花岗闪长斑岩体,找矿潜力巨大。

关 键 词:铜钼多金属矿床  矿床地质特征  花岗闪长斑岩  辉钼矿  格咱岛弧

Geochemical characteristics and geological significance of Tongchanggou Cu-Mo polymetallic deposit in Gezan Island Arc of Yunnan
Abstract:This paper analyzed the geochemical elements of granodiorite-porphyry in Tongchanggou mining area and the geological characteristics of the mining area.The results revealed the contents of granodiorite-por-phyry in this area,which include SiO 2 (66.32%-69.60%),Al2 O 3 (14.05%-15.55%),and MgO (1.1 9%-1.39%).The A/CNK value ranges from 0.88-1.05,and it indicates that the granodiorite-porphyry is a kind of metaluminous to weakly peraluminous rock.With K2 O + Na2 O content accounting for 6.97%-9.1 1%,the alkalinity of the rocks is higher than that of intermediate-acidic rocks.The rock is LREE en-riched (LREE/HREE=13.56-1 6.94)and is characterized by obvious fractionation between light and heavy rare earth elements (LaN/YbN =25.97-36.73).The values ofδEu (0.87-1.01)andδCe (0.89-0.94)in-dicate no significant anomalies.The rock is characterized by LILE (short for large ion lithophile element,in-cluding Rb,K,La,Ba)enrichment and HFSE (high field strength element,including Nb,Hf,Ti)deple-tion,which suggests that it is a kind of orogenic granite series related to the plate subduction.The porphyry orebodies in the deposit are closely related to the mineralization after magmatic intrusion,and skarn type and hydrothermal vein type orebodies are correlated with upward intrusion and filling of magmatic hydrothermal fluid and contact metasomatism.The projects at the deep part of the mining area have revealed the existence of concealed granodiorite-porphyry rock bodies at depth and the deposit has great prospecting potential.
Keywords:Cu-Mo polymetallic deposit  geological characteristic of deposit  granodiorite-porphyry  molyb-denite  Gezan Island Arc
本文献已被 CNKI 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号