| 江西省莲花县江下垅粉石英矿地质特征及找矿方向 |
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| 引用本文： | 李健,王绍奇. 江西省莲花县江下垅粉石英矿地质特征及找矿方向[J]. 上海国土资源, 2010, 31(Z1) |
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| 作者姓名： | 李健 王绍奇 |
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| 作者单位： | 江西省地质矿产勘查开发局九○一地质大队,江西萍乡,337000 |
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| 摘 要： | 江西省莲花县江下垅粉石英矿,赋存于二叠系上统狮子形组,系硅质灰岩、硅质岩风化而成。矿体严格受地层控制,岩石硅质成分是成矿的先决条件,温暖湿润的气候是成矿的后天条件。
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| 关 键 词： | 硅质灰岩 粉石英 |
The Geological Characteristics and Prospecting Direction of Jiangxialong Konilite Deposit in Lianhua County,Jiangxi Province |
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| LI Jian,WANG Shao-Qi. The Geological Characteristics and Prospecting Direction of Jiangxialong Konilite Deposit in Lianhua County,Jiangxi Province[J]. Shanghai Land & Resource, 2010, 31(Z1) |
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| Authors: | LI Jian WANG Shao-Qi |
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| Affiliation: | LI Jian,WANG Shao-Qi (No.901 Geological Party of Jiangxi Bureau of Geology Exploration,Jiangxi Pingxiang 337000,China) |
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| Abstract: | Jiangxialong konilite deposit in Lianhua county,Jiangxi province occurrences in the lion formation of Permian system,which is weathering from siliceous limestone & siliceous rock.,Ore is controlled strictly by stratum,the siliceous component of rock is the precondition of mineralization,warm and moist climate is the postnatal conditions of mineralization. |
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| Keywords: | siliceous limestone konilite |
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