夹皮沟金矿田脉岩与矿体的关系

J4 ›› 2001, Vol. 9 ›› Issue (2): 7-11.

夹皮沟金矿田脉岩与矿体的关系

綦远江,杨文风,赵琪

吉林有色地质勘查院604分院, 吉林　桦甸　132400

收稿日期:2000-12-25 修回日期:2001-04-03 出版日期:2001-04-28 发布日期:2011-10-28
作者简介:綦远江(1964-),地质工程师,主要从事找矿勘探与研究.

The Relation ship between the orebodies and the dikes in Jiapigou Gold Ore Field

QI Yuan-jiang,YANG Wen-feng,ZHAO Qi

604 Branch of Geologic Survey for Nonferrous Metal Resources in Jilin,Huadian Jilin 132400, China

Received:2000-12-25 Revised:2001-04-03 Online:2001-04-28 Published:2011-10-28

摘要/Abstract

摘要：

夹皮沟花岗岩—绿岩带内脉岩种类繁多、规模不一、形成有先有后, 但它们与含金流体之间具空间一致、时间上交叉形成。脉岩的岩性与围岩岩性对成矿作用影响很大, 通过分析, 揭示了暗色岩系中浅色脉岩与矿体关系密切和浅色岩系中暗色脉岩与矿体关系密切的原因。

关键词: 脉岩, 矿体, 金矿田, 夹皮沟

Abstract:

The dikes in Jiapigou granulaite-grecnstone belt,characted by different kinds,scales,as well as times,corresponded to and alternated with gold-bearing fluid on space and time reprcsen tatively.Them ineralizations were influenced strongly by the properties of dikes and wall rocks.Analysis shows the reason why the ore bodies are closely related to both light-coloured dikes in dark-coloured rock series and dark-coloured dikes in light-coloured rock series.

Key words: Dike, orebody, gold ore field, Jiapigou

中图分类号:

P681.01/P618.51

綦远江,杨文风,赵琪. 夹皮沟金矿田脉岩与矿体的关系[J]. J4, 2001, 9(2): 7-11.

QI Yuan-jiang,YANG Wen-feng,ZHAO Qi. The Relation ship between the orebodies and the dikes in Jiapigou Gold Ore Field[J]. J4, 2001, 9(2): 7-11.

参考文献

[1] 丁式江.胶东焦家金矿蚀变岩中元素质量迁移[J].地质与勘探,2000,36(4).
[2] 程玉明.吉辽地区绿岩带金矿成矿找矿模式[M].北京:地震出版社,1996.

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