| 松山-石山断隆小而富金矿床的地质特征及成因探讨 |
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| 引用本文： | 宋雨春,冯国清,春乃芽.松山-石山断隆小而富金矿床的地质特征及成因探讨[J].有色矿冶,2004,20(6):4-6. |
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| 作者姓名： | 宋雨春 冯国清 春乃芽 |
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| 作者单位： | 辽宁省有色地质局葫芦岛地质勘查院,辽宁,葫芦岛,125000 |
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| 摘 要： | 松山-石山断隆位于山海关-北镇隆起带中部，具有花岗岩一绿岩的构造体制．即在低变质区中分布有金矿床。该断隆上的金矿床产于太古界建平群老变质杂岩系中，金矿床严格受断裂构造控制。矿化类型为含金石英脉型。矿体规模小．埋藏浅、品位高。
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| 关 键 词： | 松山——石山断隆 小而富金矿床 地质特征 成矿作用分析 |
| 文章编号： | 1007-967X(2004)06-0004-03 |
| 修稿时间： | 2004年3月23日 |
The Geological Characteristic and Genesis Research of the Small Scale and High-grade Au-ore in Songshan-shishan Anteclise |
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| SONG Yu-chun,FENG Guo-qing,CHUN Nai-ya.The Geological Characteristic and Genesis Research of the Small Scale and High-grade Au-ore in Songshan-shishan Anteclise[J].Non-Ferrous Mining and Metallurgy,2004,20(6):4-6. |
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| Authors: | SONG Yu-chun FENG Guo-qing CHUN Nai-ya |
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| Abstract: | Songshan-shishan anteclise located in the middle parts of the Shanhaiguan-beizhen umbones was characterized by the granite-greenstone structure system i.e. the low-grade metamorphic zones have hosted the gold ore deposits occurring in the old metamorphic complex rocks in the Archean Erathem Jianping group,and the gold-bearing quartz veins type ore deposits strictly controlled by the fractures have specific characteristic of the shallow-buried and smallscale but high-grade orebodies. |
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| Keywords: | Songshan-shishananteclise small scale & high-grade Au ore geological characteristic ore-forming process analysis |
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