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平庄盆地NNE、EW向断裂构造对地下水的控制特征

Groundwater Controlling Features of NNE and EW Faulted Structures in Pingzhuang Basin

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【作者】 刘大野刘民娟唐学民李明宫卫民

【Author】 Liu Daye1, Liu Minjuan1, Tang Xuemin1, Li Ming2, Gong Weimin3 (1.The 104 Team, Inner Mongolia Bureau of Coal Geology, Chifeng, Inner Mongolia 024076; 2. Testing and Research Center, Northeast China Bureau of Coal Geology, Shenyang, Liaoning 10015; 3. Foundation Engineering Company, Northeast China Bureau of Coal geology, Shenyang, Liaoning 110015)

【机构】 内蒙古煤田地质局104队东北煤田地质局测试研究中心东北煤田地质局基础工程公司 内蒙古赤峰024076内蒙古赤峰024076辽宁沈阳110015辽宁沈阳110015

【摘要】 依据地质资料,讨论了平庄盆地NNE—EW向断裂构造对地下水的控制特征。其结论是:富水的是EW向张性断裂构造,断裂构造的富水程度固有多种原因,但主要是于现今地应力场作用下所形成的断裂力学性质及其活动性,至关重要。掌握断裂构造对地下水的控制特征。对于分析和寻找地下水资源,无疑是有意义的。

【Abstract】 According to geological data, the paper discussed groundwater-controlling features of NNE and EW faulted structures in Pingzhuang basin. The findings are:EW tensional faulted structures are water-rich, there are diversified reasons of the conclusion,but the most important main reason is mechanical property and activity of faulted structures formed under earth stress field on the stage.To know well the water controlling features of faulted structures is meaningful in analyses and finding of groundwater resources.

  • 【文献出处】 中国煤田地质 ,Coal Geology of China , 编辑部邮箱 ,2004年05期
  • 【分类号】P641.135
  • 【被引频次】8
  • 【下载频次】126
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