| 江西云山地区邓家山锡矿床地质特征 |
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| 引用本文： | 朱汗青.江西云山地区邓家山锡矿床地质特征[J].福建地质,2006,25(1):25-31. |
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| 作者姓名： | 朱汗青 |
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| 作者单位： | 中国地质大学,武汉,430074;江西地矿局916大队,九江,332100 |
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| 基金项目： | 江西省地质矿产局,1：20万永修幅区域地质矿产调查报告,1973.本文成文过程中,得到汪石林教授级高级工程师,周开朗、朱冬梅高级工程师的审阅和指导,薛志华绘制了有关插图,在此表示感谢! |
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| 摘 要： | 重点介绍了江西云山地区邓家山锡矿床的地质特征,初步探讨了矿床成因及找矿标志。邓家山锡矿成矿作用主要受后期北北东向构造蚀变带控制,主要矿化类型为构造蚀变岩带型。成因类型属高-中温热液交代-充填型矿床为主。
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| 关 键 词： | 锡矿床 地质特征 找矿标志 邓家山 |
| 收稿时间： | 2004-01-15 |
| 修稿时间： | 2004年1月15日 |
Geologic Characteristics of the Dengjiashan Tin Deposit in the Yunshan Arae of Jiangxi Province |
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| Zhu Hanqing.Geologic Characteristics of the Dengjiashan Tin Deposit in the Yunshan Arae of Jiangxi Province[J].Geology of Fujian,2006,25(1):25-31. |
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| Authors: | Zhu Hanqing |
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| Institution: | China University of Geosciences , Wuhan, 430074 |
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| Abstract: | The paper presents the geologic characteristics of the Dengjiashan tin deposit in the Yuashan area of Jiangxi Province and the ore-forming cause and ore-hunting indicators for the tin deposit are also under discussion herein.It is inferred that the ore-forming process of the Dengjiashan tin deposit is mainly controlled by the late-stage tectonic altered zones with the NNE trend and the major metallization pattern is the type of the tectonic altered rock zone.The genetic type of the deposit belongs to the hypothermal and mesothermal replacement pattern. |
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| Keywords: | tin deposit geologic characteristics ore-hunting indicator Dengjianshan(area) |
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