| 辽宁兴城元台子银铅锌多金属矿成矿条件及找矿前景 |
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| 引用本文： | 裴蕾,王永春,方磊,刘思青.辽宁兴城元台子银铅锌多金属矿成矿条件及找矿前景[J].地质找矿论丛,2015,30(3):337-343. |
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| 作者姓名： | 裴蕾 王永春 方磊 刘思青 |
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| 作者单位： | 辽宁工程技术大学矿业学院, 辽宁阜新 123000;辽宁工程技术大学矿业学院, 辽宁阜新 123000;辽宁省核工业地质勘查院, 沈阳 110000;中国科学院南海海洋研究所边缘海重点实验室, 广州 510301;中国科学院大学, 北京 100049 |
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| 摘 要： | 元台子银铅锌多金属矿位于兴城首山—大英昌—杨家杖子NW向断裂带与黑风山—梁家沟—季家沟NE向断裂带的交汇部位。银铅锌多金属矿体主要赋存于长城系常州沟组石英岩与燕山早期花岗岩的接触带中,矿体多呈似层状、脉状产出,为热液充填型矿床,成矿与断裂构造与岩浆热液的活动关系密切。该区成矿地质条件优越,是银、铜、钼、铅锌等金属元素的富集区域,找矿潜力较大。
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| 关 键 词： | 元台子银铅锌多金属矿 断裂构造 燕山早期花岗岩 热液充填型 成矿条件 辽宁省 |
| 收稿时间： | 2014/6/20 0:00:00 |
Metallogenic conditions and prospecting potential of the Yuantaizi Ag-Pn-Zn polymetallic deposit in Xingcheng county, Liaoning province |
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| PEI Lei,WANG Yongchun,FANG Lei and LIU Siqing.Metallogenic conditions and prospecting potential of the Yuantaizi Ag-Pn-Zn polymetallic deposit in Xingcheng county, Liaoning province[J].Contributions to Geology and Mineral Resources Research,2015,30(3):337-343. |
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| Authors: | PEI Lei WANG Yongchun FANG Lei and LIU Siqing |
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| Institution: | College of Mining, Liaoning Technology University, Fuxin 123000, China;College of Mining, Liaoning Technology University, Fuxin 123000, China;Liaoning Nuclear Industry Geological Prospecting Institute, Shenyang 110000, China;Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;University of Chinese Academy of Sciences, Beijing 100049, China |
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| Abstract: | The Yuantaizi Ag-Pn-Zn polymetallic deposit is located at the intersection of NW Shoushan Mountain-Dayingchang-Yangjiazhangzi fault zone and NE Heifengshan Mountain-Liangjiagou-Jijiagou fault zone in Xingcheng county. Genetically, it is a hydrothermal filling deposit and ore bodies are layeroid or vein like. On basis of the geological characteristics and geophysical analysis are elaborated metallogenic condition and prospecting potential in the area. Ore bodies occur mainly in the contact of quartzite in Changzhougou formation of Changcheng system and the Early Yanshanian granite intrusion and are closely related to the multiple tectonic activities of the main fault zone and magmatic hydrothermal activities. The metallogenic geological conditions are superior and Ag, Cu, Pb, Zn etc. are concentrated thus here is potential for further prospecting. |
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| Keywords: | Yuantaizi Ag-Pn-Zn polymetallic ore fault structure Early Yanshanian granite intrusion hydrothermal filling type metallogenic geological condition Liaoning province |
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