| 建平烧锅营子金矿区成矿构造—岩浆控制 |
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| 引用本文： | 郑超,王建国,赵纯福,马民涛,黄菲,郝辉.建平烧锅营子金矿区成矿构造—岩浆控制[J].材料与冶金学报,1995(1). |
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| 作者姓名： | 郑超 王建国 赵纯福 马民涛 黄菲 郝辉 |
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| 基金项目： | 国家黄金局地质科研项目 |
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| 摘 要： | 烧锅营子地区金矿的形成主要是由构造活动、岩浆侵入和围岩蚀变等成矿控制因素综合作用的结果，东西向构造带严格控制着金矿带、金矿床呈等距离展布，与其具有成生联系的次级东西向、北东向和北西向断裂又是含金矿脉的主要容矿构造．合金矿脉皆产于岩体边缘相地带，且与细粒闪长岩脉相伴而存，表明脉岩矿脉于空间上、时间上及成因上和燕山期黑云母花岗岩浆的演化活动有关，三者为同源关系．
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| 关 键 词： | 成矿控制 构造活动 岩浆侵入 |
On Minerogenetic Structure in Jianping Shaoguoyingzi Gold Deposit-Magma Control |
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| Zhen Chao, Wang Jianguo et al.On Minerogenetic Structure in Jianping Shaoguoyingzi Gold Deposit-Magma Control[J].Journal of Materials and Metallurgy,1995(1). |
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| Authors: | Zhen Chao Wang Jianguo |
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| Affiliation: | Department of Geology |
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| Abstract: | The formation of the gold deposits in Shaoguoyingzi area is the comprehensive results of such ore-control factors as structural activities, magma intrusion and wall rock alteration. The evenly distributed ore zones and deposits are strictly controlled by EW structural zones. The secondary EW, NE and NW fractures are the main hosting structures for gold bearing veins. The gold bearing veins oeeur in the rock of border facies and coexist with fine-grained dioritic veins, which shows that the ore veins, rock veins are related in time, space and genesis with the evolution of Yanshanian biotite-granitic magma, and are cognate. |
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| Keywords: | minerogenetic control structural activity magma intrusion |
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