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海阳东刘家地区金矿化特征及成矿模式探讨
引用本文:高长亮,张春池,王星远,刘书锋,王继增,郑作平.海阳东刘家地区金矿化特征及成矿模式探讨[J].山东国土资源,2001(Z1).
作者姓名:高长亮  张春池  王星远  刘书锋  王继增  郑作平
作者单位:山东省第一地质矿产勘查院 山东济南250014 (高长亮,张春池,王星远,刘书锋,王继增),山东省第一地质矿产勘查院 山东济南250014(郑作平)
摘    要:通过对东刘家地区金矿床地质特征的分析研究 ,认为该区金矿床受层间滑动构造系统控制 ,赋存于古元古代荆山群或侵入其中的二长花岗岩之中 ,其矿床成因为多源多期中低温热液型。

关 键 词:金矿  矿床特征  层间滑动  成矿模式  山东海阳

Study on Gold Mineralization Characteristics and Ore-forming Model in Dongliujia Area of Haiyang City
GAO Chang-liang,ZHANG Chun-chi,WANG Xing-yuan,LIU Shu-feng,WANG Ji-zeng,ZHENG Zuo-pin.Study on Gold Mineralization Characteristics and Ore-forming Model in Dongliujia Area of Haiyang City[J].Land and Resources in SHANDONG Province,2001(Z1).
Authors:GAO Chang-liang  ZHANG Chun-chi  WANG Xing-yuan  LIU Shu-feng  WANG Ji-zeng  ZHENG Zuo-pin
Abstract:Through the study on geological characteristics of gold deposits in Dongliujia area, it is regarded that gold deposits are controlled by interbedded slip fault system and occurred in Jingshan group of Palaeo-proterozoic or monzonitic granite intruded into the group. The genesis of gold deposits belong to muiti-sources and polyphase hydrothermal type.
Keywords:Gold deposit  geological characteristics  interbedded slide  ore-forming model  Dongliujia area in Haiyang city
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