云西矿床9 号糜棱岩带的控矿容矿构造初探

J4 ›› 2003, Vol. 11 ›› Issue (4): 6-11.

云西矿床9 号糜棱岩带的控矿容矿构造初探

李新福

广东高要河台金矿, 广东高要 526127

收稿日期:2002-11-12 修回日期:2003-05-19 出版日期:2003-08-30 发布日期:2011-11-24
作者简介:李新福(1972-), 男, 助理工程师, 从事岩金矿山地质的技术与管理工作.

PROMARY STUDY ON THE ORE-CONTROLLING AND ORE-CONTAINING TECTONIC OF NO.9 MYLONITE ZONE OF YUNXI GOLD DEPOSIT

LI Xinfu

Hetai Gold Mine, Gaoyao, Guangdong. Guangdong Gaoyao 526127, China

Received:2002-11-12 Revised:2003-05-19 Online:2003-08-30 Published:2011-11-24

摘要/Abstract

摘要：

河台金矿云西矿床作为多源热液糜棱岩型金矿床, 在糜棱岩形成过程的中后期由韧性剪切变为张性剪切而产生的一系列控矿和容矿构造对矿体的形成有重要的作用。这些构造对矿体的产出空间、位置和产出形态起着控制作用, 研究其规律为今后探矿将具有指导意义。

关键词: 云西矿床, 多源热液糜棱岩型金矿床, 控矿构造, 容矿构造

Abstract:

Yunxin gold deposit of Hetai Gold Mine plays an important role in the forming of mine body as a multiple source hydrothermal mylonite gold deposit, during the mylonite forming, a serial of ore-controlling & ore-containing happened in its late period from ductile shear to tensile shear. These tectonic control the production space, position& production pattern of the mine body; study its regulation to guide our future prospecting

Key words: Yunxi deposit multiple source hydrothermal, mylonite gold deposit, ore-controlling tectonic, ore-containing tectonic

中图分类号:

P618.5102

李新福. 云西矿床9 号糜棱岩带的控矿容矿构造初探[J]. J4, 2003, 11(4): 6-11.

LI Xinfu. PROMARY STUDY ON THE ORE-CONTROLLING AND ORE-CONTAINING TECTONIC OF NO.9 MYLONITE ZONE OF YUNXI GOLD DEPOSIT[J]. J4, 2003, 11(4): 6-11.

参考文献

[1] 王鹤年, 张景荣, 陆建军, 等. 粤西金矿床地球化学. 南京: 南京大学出版社. 1991.
[2] 周永章. 广东高要河台金矿地球化学及成矿机理. 广东地质, 1993,(4): 13-17.
[3] 原广东省地矿局719 地质队. 广东高要云西矿床地质勘探报告.(内部资料), 1993.

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