| 扬子地块西北缘、西南缘卡林型金矿床的构造控矿特征 |
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| 引用本文： | 谭运金.扬子地块西北缘、西南缘卡林型金矿床的构造控矿特征[J].岩土工程界,1997(3). |
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| 作者姓名： | 谭运金 |
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| 作者单位： | 有色总公司矿产地质研究院 |
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| 摘 要： | 扬子地块西北缘、西南缘卡林型金矿床的构造控矿特征主要表现为：被动大陆边缘裂谷（裂陷）带是含金建造形成的区域构造背景；逆冲推覆构造是成矿元素和成矿流体活化、迁移、富集成矿的重要热动力；低级别、低序次的断裂和密集裂隙带是成矿流体的通道和矿体的定位空间。
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| 关 键 词： | 控矿构造 卡林型金矿床 扬子地块 |
ORE CONTROLLING STRUCTURES OF THE SEDIMENTS HOSTED DISSEMINATED GOLD DEPOSIT IN THE NORTH WEST AND SOUTH WEST MARGINS OF THE YANGTZE PLATE |
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| Tan Yunjin.ORE CONTROLLING STRUCTURES OF THE SEDIMENTS HOSTED DISSEMINATED GOLD DEPOSIT IN THE NORTH WEST AND SOUTH WEST MARGINS OF THE YANGTZE PLATE[J].Geotechnical Engineering World,1997(3). |
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| Authors: | Tan Yunjin |
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| Abstract: | The ore controlling structure of the sediments hosted disseminated gold deposit in north west and south west margins of the Yangtze plate is mainly summarized as:the rift basin developed along the passive continental margin of the Yangtze plate being the regional tectonic setting of gold bearing formation;thrust nappe fault providing thermodynamic power for mobilization and transportation of ore forming elements and fluid;the lower order fractures playing roles of the passway of fluid and the positional space of ores. |
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| Keywords: | Ore controlling structure sediments hosted disseminated gold deposit north west and south west margins of the Yangtze plate |
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