| 董泽龙,张随波,白永俊,王泽,李雪松.辽宁省红旗营子铅锌矿床岩脉与含矿构造关系研究[J].地质找矿论丛,2013,28(4):570-575 |
| 辽宁省红旗营子铅锌矿床岩脉与含矿构造关系研究 |
| Research on the relationship between dyke in Hongqiyingzi Pb-Zn deposit in Liaoning province and the mineralized structure |
| 投稿时间：2013-05-21 |
| DOI：10.6053/j.issn.1001-1412.2013.04.012 |
| 中文关键词: 红旗营子铅锌矿 含矿构造 岩脉 地质意义 辽宁省 |
| 英文关键词:Hongqiyingzi Pb-Zn deposit mineralized structure dyke geological significance Liaoning |
| 基金项目: |
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| 摘要点击次数: 2029 |
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| 中文摘要: |
| 文章通过野外对岩脉和含矿构造特征的观察研究，得出它们之间的先后顺序为：NE向花岗斑岩脉→闪长玢岩→矿化构造，NW向岩脉最晚。早期的NE向岩脉为成矿物质提供了运移通道和最佳的容矿空间，并表现为构造矿化带常沿着岩脉产出。 |
| 英文摘要: |
| Observation and study on geological characteristics of dykes and mineralized structures in Hongqiyingzi Pb-Zn deposit show the sequence of NE granite porphyry dyke→diorite porphyrite-→mineralized structure→NW dyke. The early NE granite porphyry dyke serves as optimum transportation channel of ore fluid and ore hosting space. On the spot of the deposit the structural-mineralized zones generally stretch along the early NE dyke. |
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