| 铜陵地区深埋型岩溶形成机制及分布特征 |
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| 引用本文： | 丁有全.铜陵地区深埋型岩溶形成机制及分布特征[J].水文地质工程地质,1997,24(1):43-45. |
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| 作者姓名： | 丁有全 |
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| 作者单位： | 安徽地矿局321地质队!铜陵244033 |
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| 摘 要： | 铜陵地区现代岩溶发育深度一般在２００ｍ以内，但在特殊地质块段存着埋藏深度更大的岩溶，它的存在对地下水资源的开采和深埋矿床的开采具有重要意义，该类岩溶按成因可分为岩浆侵入型，断裂构造型和古岩溶，本文就其形成机制和分布特征进行了探讨。
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| 关 键 词： | 岩溶 形成机制 成因分类 分布特征 岩溶发育 |
Formation mechanism and distribution of deep-lying karst in Tongling area |
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| Dying Youquan.Formation mechanism and distribution of deep-lying karst in Tongling area[J].Hydrogeology and Engineering Geology,1997,24(1):43-45. |
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| Authors: | Dying Youquan |
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| Institution: | Dying Youquan |
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| Abstract: | In Tongling area. the modern karst is formed at the depth of 200m, but still deeper karsts are hidden in special sections of the area, which are worth of notice for the mining of groundwater resources and deep-lying deposits. These karsts could be divided into magma intrusive, fault structural and palaeokarst according to their genesis. This paper discusses the formation mechanism and distribution characteristics of these karsts. |
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| Keywords: | deep-lying karst formation mechanism genetic classification |
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