| 湖南城步县金水铜矿地质特征及成因探讨 |
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| 引用本文： | 谢新泉,张衡龙.湖南城步县金水铜矿地质特征及成因探讨[J].华南地质与矿产,2005(1):37-40. |
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| 作者姓名： | 谢新泉 张衡龙 |
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| 作者单位： | 湖南省地勘局407队,湖南,怀化,418000 |
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| 基金项目： | 中国地调局国土资源大调查项目(200210200047). |
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| 摘 要： | 金水铜矿床受构造控制,热液成矿标志明显。依据成矿地质背景及矿床地质特征、硫同位素和流体包裹体特征等研究认为,成矿物质来源深部,成矿作用具多阶段,成矿流体具热卤水性质;矿床初步确定为岩浆期后热液脉型铜矿床。
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| 关 键 词： | 铜矿床 层间破碎带 岩浆热液 湖南城步 |
| 文章编号： | 1007-3701(2005)01-0037-04 |
| 修稿时间： | 2004年5月20日 |
Geological characteristics and genesis of the Jinshui copper deposit in Chengbu County,Hunan Province |
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| XIE Xin-quan,ZHANG Heng-long.Geological characteristics and genesis of the Jinshui copper deposit in Chengbu County,Hunan Province[J].Geology and Mineral Resources of South China,2005(1):37-40. |
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| Authors: | XIE Xin-quan ZHANG Heng-long |
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| Abstract: | The Jinshui copper deposit is controlled by structures and show obvious characteristics of hydrothermal origin. Study on metallogenetic backgrounds,geology of ore deposit,sulphur isotopes and fluid inclusions of main minerals shows that the metallogenetic materials came from the deep crust and mineralization fluids might be hot brine. The deposit endured multi-stage mineralization and belongs to a post-magmatic hydrothermal copper deposit. |
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| Keywords: | copper deposit intralayer fracture zone magmatic hydrothermal Chengbu Hunan Province |
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