| 郴州市金船塘锡铋矿床地质特征及成矿规律探讨 |
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| 引用本文： | 陈荣华 刘昌新. 郴州市金船塘锡铋矿床地质特征及成矿规律探讨[J]. 湖南地质, 1997, 16(2): 101-105 |
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| 作者姓名： | 陈荣华 刘昌新 |
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| 作者单位： | 地矿部湖南省地质矿产勘查开发局，湘南地质勘察院 |
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| 摘 要： | 金船塘矿区位于南岭多金属成矿带中段北缘，千里山花岗岩体外接触带。属产于中上泥盆统的矽卡岩型锡铋矿床，构造、岩性和岩浆活动联合控矿，锡铋矿的成生与矽卡岩化蚀变密切相关。
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| 关 键 词： | 锡矿床 铋矿床 地质特征 成矿规律 |
Jinchuantang Sn-Bi Deposit in Chengzhou City and its Metallogeny |
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| Chen Ronghuo Liu Changxing Xu ShiguangInsitute of Geology and Exploration of South Hunan,HBGMR. Jinchuantang Sn-Bi Deposit in Chengzhou City and its Metallogeny[J]. Land & Resources Herald, 1997, 16(2): 101-105 |
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| Authors: | Chen Ronghuo Liu Changxing Xu ShiguangInsitute of Geology Exploration of South Hunan HBGMR |
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| Abstract: | Lying in the North margin of the middle section of Nanling metallogenic belt and at the outer part of the contact zone betweem Qianlishan Granite and the limestone,Jinchuantang deposit is a skarn Sn-Bi deposit,occurring in strata of the Middle-Upper Devonian systern and being controlled by structure,rock feature and magamatic activity all together.Mineralization is related closely to skarn alteration. |
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| Keywords: | Sn-Bi deposit skarnization metallogeny prospecting area Chengzhou |
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