| 神府矿区活鸡兔矿井烧变岩水文地质特征 |
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| 引用本文： | 牛建国.神府矿区活鸡兔矿井烧变岩水文地质特征[J].煤田地质与勘探,2001,29(1):37-39. |
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| 作者姓名： | 牛建国 |
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| 作者单位： | 陕西煤田地质局185队 |
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| 摘 要： | 烧变岩是活鸡兔矿井的顶板充水含水层，直接威胁着矿井的生产安全，烧变岩分布广泛，裂隙发育程度在垂向规律明显，下剧－中强－上弱，其富水性除受构造，地形地貌的控制外，还决定于是否接受其他含水层的补级，煤变岩水水质良好，符合国家饮用水标准，供排结合是矿井水综合利用的有效方法。
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| 关 键 词： | 烧变岩 水文地质条件 矿井 含水层 裂隙发育程度 成因 防治 利用 |
| 文章编号： | 1001-1986(2001)01-0037-02 |
| 修稿时间： | 1999年12月17 |
Hydrogeological characteristics of burnt rock in Huojitu Mine,Shenfu Mining Area |
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| NIU Jian-guo.Hydrogeological characteristics of burnt rock in Huojitu Mine,Shenfu Mining Area[J].Coal Geology & Exploration,2001,29(1):37-39. |
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| Authors: | NIU Jian-guo |
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| Abstract: | The coal seam roof of Huojitu Mine is the burnt rock,which is the water impregnated aquifer,is dangerous to mine safety.The burnt rock distributed widely.The regularities of fracture development are vertically apparant,for example,the fractrues decrease upwards.The water abundance of the rock is controlled not only by structures,geographic and surface features,but also controlled by the recharge condition from other aquifer.The water quality of the rock can meet the drinking water standards of the state.Therefore,the water control combining dewatering and water supply is the effective way. |
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| Keywords: | burnt rock hydrogeological conditions Huojitu Mine |
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