| 迂里矿段铜铅锌银多金属矿体地质特征及其矿床成因 |
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| 引用本文： | 王友谊.迂里矿段铜铅锌银多金属矿体地质特征及其矿床成因[J].地质学刊,2005,29(1):14-17. |
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| 作者姓名： | 王友谊 |
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| 作者单位： | 苏州市小茅山铜铅锌矿 江苏苏州215163 |
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| 摘 要： | 苏州迂里矿区位于苏州西部太湖之滨，其中迂里矿段铜、铅、锌、银多金属矿体具有埋藏较深，规模较小，品位较高及可综合利用元素较多的特点。矿体受地层岩性、构造、岩体等因素控制，确定了成矿的5个规律。
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| 关 键 词： | 成矿规律 褶皱 断层 苏州迂里 |
| 文章编号： | 1003-6474(2005)01-0014-04 |
| 修稿时间： | 2004年10月10 |
Cu-Pb-Zn-Ag polymetallic ore bodies in Yuli block and their geological properties and genesis |
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| WANG You,yi.Cu-Pb-Zn-Ag polymetallic ore bodies in Yuli block and their geological properties and genesis[J].Jiangsu Geology,2005,29(1):14-17. |
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| Authors: | WANG You yi |
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| Abstract: | Yuli ore block lies in Guangfu town,west of Suzhou city,near Taihu lake,22.5km from the urban downtown of Suzhou.Yuli ore block vests in the foreland basin of Dean to Suzhou along the north stretches of Jiangnan uplift in terms of regional tectonics,and southeast Anhui to Taihu fold to Suzhou composite syncline belt.Yuli ore block extends NNE and falls into three blocks of Guangfu,Hushan and Yuli from south to north.The ore blocks for Guangfu and Husan are low in exploration degree and Yili ore block is mostly discussed here in the text.The polymetallic ore bodies like copper,lead,zinc and silver are characteristic of deep burial,small scale,high grade and many useful elements.The ore bodies are controlled by strata lithology,structures,rock masses.Five metallogenic rules are determined and their genesis is explained. |
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| Keywords: | Metallogenic rules Folds Faults Yuli Suzhou Jiangsu |
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