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吉林海沟金矿地质特征及应力场分析
引用本文:冯明,曹成润,陈力,董晓伟.吉林海沟金矿地质特征及应力场分析[J].地质与资源,2005,14(4):268-271.
作者姓名:冯明  曹成润  陈力  董晓伟
作者单位:1. 吉林大学地球科学学院, 吉林长春 130061;2. 吉林大学建设工程学院, 吉林长春 130026
基金项目:国家重点基础研究发展规划973项目(2003CB211708)资助.
摘    要:海沟金矿是大型石英脉型金矿床,矿体严格受NE向断裂构造控制,成矿时代为晚侏罗世-早白垩世.矿石中金属矿物以黄铁矿、自然金、方铅矿和黄铜矿为主.28号主矿脉中,Au平均品位20.59×10-6.成矿物质来自地层和岩体.对构造应力场研究表明,矿区有3期构造应力场,分别是早期近S-N向挤压、中期NW向挤压和晚期NE向挤压.成矿期应力场最大主压应力方向为NE向.

关 键 词:海沟金矿  构造应力场  石英脉  地质特征  
文章编号:1671-1947(2005)04-0268-04
收稿时间:2004-12-20
修稿时间:2005-02-24

GEOLOGIC CHARACTERISTICS AND TECTONIC STRESS FIELD OF HAIGOU QUARTZ-VEIN GOLD DEPOSIT IN JILIN PROVINCE
FENG Ming,CAO Cheng-run,CHEN Li,DONG Xiao-wei.GEOLOGIC CHARACTERISTICS AND TECTONIC STRESS FIELD OF HAIGOU QUARTZ-VEIN GOLD DEPOSIT IN JILIN PROVINCE[J].Geology and Resources,2005,14(4):268-271.
Authors:FENG Ming  CAO Cheng-run  CHEN Li  DONG Xiao-wei
Institution:1. College of Earth Science, Jilin University, Changchun 130061, China;2. College of Construction Engineering, Jilin University, Changchun 130026, China
Abstract:Haigou gold deposit in Jilin province is of a large quartz vein type. The ore bodies are strictly controlled by NE-trending fault structures.The ore-forming period ranges from Late Jurassic to Early Cretaceous.The metal mineral s in ore are mainly pyrite,native gold,chalcopyrite and galena.The average grade of gold in the main ore vein is 20.59 ×10-6.Tectonic stress field analysis in dicates that in the gold field,there are 3 tectonic stress stages,namely,the ear ly style of S-N-trending compression,the middle stage of NW-trending compress ion and the last stage of NE-trending compression.
Keywords:Haigou gold deposit  tectonic stress field  quartz vein  geologic characteristics
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