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迂里矿段铜铅锌银多金属矿体地质特征及其矿床成因 被引量:2

Cu-Pb-Zn-Ag polymetallic ore bodies in Yuli block and their geological properties and genesis
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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。 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.
作者 王友谊
出处 《江苏地质》 2005年第1期14-17,共4页 Jiangsu Geology
关键词 成矿规律 褶皱 断层 苏州迂里 Metallogenic rules Folds Faults Yuli,Suzhou,Jiangsu
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  • 1金哨文 范惠民 吴福昌.江苏省吴县光福镇迂里矿区铅锌银详查地质报告[R].,1991..

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