| 安妥岭斑岩型铜（钼）矿成矿条件与远景分析 |
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| 引用本文： | 柳凤娟,张喜周,沈柳生.安妥岭斑岩型铜（钼）矿成矿条件与远景分析[J].矿产与地质,2010,24(2):132-135,161. |
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| 作者姓名： | 柳凤娟 张喜周 沈柳生 |
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| 作者单位： | 1. 天津华北地质勘查总院,天津,300181
2. 河南省安阳市第七地质大队,河南,安阳,455000 |
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| 摘 要： | 安妥岭斑岩体发育在上黄旗-乌龙沟、岭南台-紫荆关两深断裂所夹持部位,属多次侵入的浅成-超浅成中酸性岩体,岩体规模较小,形态为整体向南倾、向南东侧伏的椭圆状,蚀变强烈具一定分带性;受次级近EW向韧性剪切断裂带、NE向韧-脆性断裂带、NW向横张断裂控制,这些特征均可与国内、外含矿斑岩体相类比。因此,本区斑岩型铜（钼）矿的成矿地质条件优越,具有形成大型斑岩铜（钼）矿床的成矿远景。
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| 关 键 词： | 斑岩型铜（钼）矿 成矿条件 成矿远景 安妥岭 河北 |
The metallogenic condition and prospect analysis of porphyry copper-molybdenum deposit in Antuoling |
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| LIU Feng-juan,ZHANG Xi-zhou,SHEN Liu-sheng.The metallogenic condition and prospect analysis of porphyry copper-molybdenum deposit in Antuoling[J].Mineral Resources and Geology,2010,24(2):132-135,161. |
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| Authors: | LIU Feng-juan ZHANG Xi-zhou SHEN Liu-sheng |
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| Institution: | 1. Tianjin North China Geological Exploration General Institute,Tianjin 300181;2. Geological Team 7#,Anyang,Henan 455000) |
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| Abstract: | The Antuoling porphyry body is located between the two deep fracture zones of Shanghuangqi-Wulonggou and Lingnantai-Zijingguan. It is a hypabyssal-super hypabyssal intermediate-acid magma rock of multiple intrusions with a small scale. It is integrally inclined to the south and pitched to the southeast as elliptical-shaped. It is strongly altered with the mineralization zoning. It is controlled by flexible shear fracture zones in eastwest,flexible-brittle fracture zones in northeast and cross tension fracture zones in northwest. These feathers all can be compared with ore-bearing porphyries in domestic and abroad. So the metallogenic condition is ascendant in this distinct,it is with the prospect of large-scale porphyry copper-molybdenum deposit. |
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| Keywords: | porphyry copper-molybdenum deposit metallogenic condition metallogenic prospect Antuoling Hebei |
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