| 山西省紫砂陶土矿床地质特征及成因 |
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| 引用本文： | 王启旺. 山西省紫砂陶土矿床地质特征及成因[J]. 太原理工大学学报, 2005, 36(4): 462-465 |
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| 作者姓名： | 王启旺 |
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| 作者单位： | 山西省煤炭地质公司,山西,太原,030045 |
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| 基金项目： | 该文得到了太原理工大学孙中诚教授的大力帮助和指导,在此表示衷心的感谢. |
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| 摘 要： | 主要讨论了山西省紫砂陶土的赋存层位、矿体特征、矿石的物理化学特征及生产成品的物理性能。简要的分析了矿床的成因,认为该矿床沉积形成于早二叠世晚期到晚二叠世早期半潮湿大陆气候的准平原化湖泊环境。
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| 关 键 词： | 紫砂陶土 矿床特征 成因 |
| 文章编号： | 1007-9432（2005）04-046204 |
| 收稿时间： | 2004-12-02 |
| 修稿时间： | 2004-12-02 |
Geological Feature and Genesis of the Purple Sand Syderolite Deposits |
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| WANG Qi-wang. Geological Feature and Genesis of the Purple Sand Syderolite Deposits[J]. Journal of Taiyuan University of Technology, 2005, 36(4): 462-465 |
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| Authors: | WANG Qi-wang |
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| Abstract: | This paper mainly discusses the layer of occurrence of purple sand sydrolite, feature of its orebody, physical-chemical feature of its ore,physic characteristics of its product. The genesis of deposits is analyzd that deposits were formed in peneplain lake condition in semi-humid continental climate during late period of early Permian and early period of late Permian. |
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| Keywords: | purple sand syderolite feature of orebody genesis |
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