宝清县团结山金铜矿床地质特征及成因探讨

J4 ›› 2006, Vol. 14 ›› Issue (4): 19-23.

宝清县团结山金铜矿床地质特征及成因探讨

许明亮^{1 , 2}, 杨建国^{1, 2} , 李远昌¹

1. 中国地质大学. 北京 100029;
2. 黑龙江省第一地质勘察院

收稿日期:2006-03-10 修回日期:2006-07-23 出版日期:2006-02-25 发布日期:2011-11-22
作者简介:许明亮(1962-), 男, 地质工程师, 主要从事地质找矿工作

The Geological Character and Genesis Analyse Of TuanJie Mountain Copper-Gold Mine In BaoQing County

XU MingLiang , YANG Jianguo , LI Yuanchang

The First Geological Reconnaissance Academy of Heilongjiang Province

Received:2006-03-10 Revised:2006-07-23 Online:2006-02-25 Published:2011-11-22

摘要/Abstract

摘要：

团结山金铜矿位于环太平洋金成矿带西侧, 完达山活动带南端的同江—虎林岩石圈断裂与大和镇壳断裂的交汇处。金铜矿化主要产于印支晚期黑云母花岗岩与大理岩、斜长角闪片岩接触形成的矽卡岩带内, 形成于矽卡岩晚期含水矽卡岩阶段。金矿(化)体的形成与铜矿化的形成同时或稍后。该成因类型是以矽卡岩为主, 辅以后期叠加热液成矿作用的金铜矿床。

关键词: 矽卡岩, 成矿作用, 成因类型

Abstract:

The TuanJie Mountain Copper-gold mine occurred in litmusless and acidic lava around Pacific Ocean in lower of Cretaceous. The ore bed exist in hot liquid breccia which has been strongly silicic and chalcedony belt. The nature gold symbiosis with quartz. In the later of volcano eruptible period, the hot liquid which carries gold to move to the ground a long the volcano channels, faultage and cranny structures. The gold that carried by the fluid is enrich to deposits where around the volcanic crater.

Key words: Skarn, Mine Effect, Kinds of Genesis

中图分类号:

P618.02

许明亮, 杨建国, 李远昌. 宝清县团结山金铜矿床地质特征及成因探讨[J]. J4, 2006, 14(4): 19-23.

HU Meng-Liang, YANG Jian-Guo, LI Yuan-Chang. The Geological Character and Genesis Analyse Of TuanJie Mountain Copper-Gold Mine In BaoQing County[J]. J4, 2006, 14(4): 19-23.

参考文献

[1] 黑龙江省宝清县团结山金铜矿详查报告(内部资料). 1998.
[2] 黑龙江省地质志. 2000.

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