| 河南省洼村粘土矿床地质特征及成因探讨 |
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| 引用本文： | 孙越英. 河南省洼村粘土矿床地质特征及成因探讨[J]. 资源调查与环境, 2005, 26(3): 199-204 |
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| 作者姓名： | 孙越英 |
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| 作者单位： | 河南省地质矿产勘查开发局第二地质队,河南焦作,454002 |
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| 摘 要： | 本文论述了洼村粘土矿床地质特征，成矿模式。根据成矿物质来源等方面研究，认为含矿岩系的物源主要来自碳酸盐岩的红土风化壳。矿床是在海侵过程中风化壳解体，经搬运、沉积、成岩及表生作用形成。
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| 关 键 词： | 粘土矿床 地质特征 成矿模式 矿床成因 河南 矿床地质特征 成因探讨 粘土 河南省 成矿物质来源 |
| 文章编号： | 1671-4814(2005)03-199-06 |
| 修稿时间： | 2004-10-11 |
Geological character and origin of Wacun clay mine in Henan |
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| SUN Yue-ying. Geological character and origin of Wacun clay mine in Henan[J]. Resources Survey & Environment, 2005, 26(3): 199-204 |
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| Authors: | SUN Yue-ying |
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| Abstract: | The geological characters and the metallogenic model of Wacun clay mine are introduced in the paper. According to the study of source of minerals etc. the ore-bearing minerals are mainly derived from the laterite weathering of carbonate rock.The deposit is formed in marine invasion by weathering crust transportation, sedimentation, diagenesis and supergenesis. |
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| Keywords: | clay mine geological character metallogenic model ore formation Wacun Henan |
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