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玲珑金矿田破头青断裂带稀土和矿化元素特征分析
引用本文:王超凡,吕古贤,郭涛,申玉科,周国发,刘维民,徐增田,刘正.玲珑金矿田破头青断裂带稀土和矿化元素特征分析[J].吉林地质,2010,29(1):99-104.
作者姓名:王超凡  吕古贤  郭涛  申玉科  周国发  刘维民  徐增田  刘正
作者单位:1. 中国地质科学院地质力学研究所,北京,100081
2. 山东黄金集团玲珑金矿,山东,招远,265419
3. 山东黄金集团烟台设计研究工程有限公司,山东,烟台,264006
基金项目:中国科学院地球化学研究所地球化学国家重点实验室开放课题 
摘    要:破头青断裂为玲珑金矿田一级控矿构造带,是重要的导矿、容矿构造;其构造蚀变分带从下盘到上盘为:钾长石化带、绢云母化带和硅化黄铁矿化带。绢英岩及其附近的钾化花岗岩、正常花岗岩的矿化元素、稀土元素分析结果表明,破头青断裂带REE配分模式表现为LREE富集型,轻、重稀土分异明显,La/Lu=8.37-65.03,具有Eu异常,δEu=0.67~1.46,Ce无明显异常;Au与Ag、As、Cu、Mo等矿化元素具有相对较高的相关性,是同一成矿作用的结果。

关 键 词:玲珑金矿  破头青断裂  稀土元素  矿化元素

Analyrsis on REE and elements related to mineralization of Potouqing fault in Linglong gold deposit
WANG Chao-fan,LV Gu-xian,GUO Tao,SHEN Yu-ke,ZHOU Guo-fa,LIU Wei-min,XU Zeng-tian,LIU Zheng.Analyrsis on REE and elements related to mineralization of Potouqing fault in Linglong gold deposit[J].Jilin Geology,2010,29(1):99-104.
Authors:WANG Chao-fan  LV Gu-xian  GUO Tao  SHEN Yu-ke  ZHOU Guo-fa  LIU Wei-min  XU Zeng-tian  LIU Zheng
Institution:1.Institute of Geomechanics,CAGS,Beijing,10081,China;2.Linglong Gold Mine of Shandong Gold Group Co.,Zhaoyuan 265419,Shandong,China;3.Shangdong Gold Group Yantai Desigh&Research Engineering CO.Ltd,Yantai,264006,Shandong,China
Abstract:Potouqing fault was the first-grade fracture controlling orebodies,its alterative zones from the hanging wall-rock to the ore-body include potash zone,sericitization zone,silicification zone,pyritation zone etc.The results of REE and elements related to mineralization in Potouqing fault show that REE patterns appear as LREE-rich type,with better fractionation of lighter and heavy REEs and La/Lu=8.37-65.03.Ore-forming fluids have Eu abnormity,withδEu=0.67-1.46 and without Ce abnormity.Au is strongly correlated to Ag,As,Cu,Mo which is the result of the same metallogeny.
Keywords:Linglong gold deposit  Potouqing faul  REE  elements related to mineralization
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