| 吉林海沟金矿地质特征及应力场分析 |
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| 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. doi: 10.13686/j.cnki.dzyzy.2005.04.007 |
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| 作者姓名： | 冯明 曹成润 陈力 董晓伟 |
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| 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 |
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| 基金项目： | 国家重点基础研究发展规划973项目（2003CB211708）资助. |
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| 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.
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| 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 |
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| 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. doi: 10.13686/j.cnki.dzyzy.2005.04.007 |
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| Authors: | FENG Ming CAO Cheng-run CHEN Li DONG Xiao-wei |
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| Affiliation: | 1.College of Earth Science, Jilin University, Changchun 130061, China;; 2.College of Construction Engineering, Jilin University, Changchun 130026, China |
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| 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. |
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| Keywords: | Haigou gold deposit tectonic stress field quartz vein geologic characteristics |
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