| 辽宁卧龙泉金矿地质特征及成因 |
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| 引用本文： | 黄海波,康志勇,温晓春.辽宁卧龙泉金矿地质特征及成因[J].地质找矿论丛,2005,20(Z1):71-74. |
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| 作者姓名： | 黄海波 康志勇 温晓春 |
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| 作者单位： | 辽宁省冶金地质勘查局,地质勘查研究院,辽宁,鞍山,114002 |
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| 摘 要： | 文章通过成矿物质来源、成矿作用与岩浆岩及构造的关系、成矿阶段的划分等方面的研究,认定卧龙泉金矿为多阶段、多成因、多来源的中-低温热液矿床.进而确定了卧龙泉金矿床的成矿模式.
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| 关 键 词： | 矿床成因 围岩蚀变 成矿作用 卧龙泉金矿 辽宁省 |
| 文章编号： | 1001-1412(2005)S0-0071-04 |
| 修稿时间： | 2005年4月6日 |
GEOLOGICAL CHARACTERISTICS AND GENESIS OF WOLONGQUAN GOLD DEPOSIT IN LIAONING PROVINCE |
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| HUANG Hai-bo,KANG Zhi-yong,WEN Xiao-chun.GEOLOGICAL CHARACTERISTICS AND GENESIS OF WOLONGQUAN GOLD DEPOSIT IN LIAONING PROVINCE[J].Contributions to Geology and Mineral Resources Research,2005,20(Z1):71-74. |
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| Authors: | HUANG Hai-bo KANG Zhi-yong WEN Xiao-chun |
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| Abstract: | On the basis of the studies of the ore-forming material sources, the ore genesis, the association of mineralization with magmatic rocks and geologic structures, stages of mineralization, etc., it is concluded that Wolongquan gold deposit is a polygenetic mesothermal or epithermal deposit formed by multiperiodic mineralization and more than one sources of ore materials. And further more, a metallogenic model is set up. |
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| Keywords: | ore genesis wallrock alteration mineralization stage of mineralization Wolongquan gold deposit Liaoning province |
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