| 张文亮,李朝辉,王亚丽.五台山区康家沟金矿床地质特征及找矿方向探讨[J].地质找矿论丛,2002,(2):116-120 |
| 五台山区康家沟金矿床地质特征及找矿方向探讨 |
| GEOLOGICAL CHARACTERISTICS OF KANGJIAGOU GOLD DEPOSIT AND ORE PROSPECT |
| 投稿时间：2001-12-17 修订日期：2002-04-01 |
| DOI：10.6053/j.issn.1001-1412.2002.2. 008 |
| 中文关键词: 绿岩带 韧性剪切带 含金石英脉 地质特征 找矿方向 五台山区 |
| 英文关键词:greenstone belt ductile shear zone Au-bearing quartz vein geological characteristics ore-searching direction Wutaishan area |
| 基金项目: |
| 作者 | 单位 | | 张文亮 | 冶金部第三地质勘查局, 地勘院, 山西, 忻州, 034000 | | 李朝辉 | 冶金部第三地质勘查局, 地勘院, 山西, 忻州, 034000 | | 王亚丽 | 冶金部第三地质勘查局, 地勘院, 山西, 忻州, 034000 |
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| 中文摘要: |
| 康家沟金矿属绿岩带型金矿。矿床(体)产于韧性剪切带中。NEE向构造为储矿(导矿)构造。矿床(体)由含金石英脉与其间蚀变岩组成,品位高低决定于含金石英脉的数量。含铁石英岩及其周围糜棱岩化带为近矿围岩。 |
| 英文摘要: |
| Kangjiagou Au deposit is a greenstone belt type deposit, controlled by shearing zone. NEN-trending structures are ore-locating structures. Ore bodies consists of Au-bearing quartz veins and the alteration rocks between them and ore grade depends on number of the quartz vein. The Au deposit is hosted in banded iron formation and in the surrounding mylonitized rock zone. |
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