| 霍州矿区断层构造的分形特征 |
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| 引用本文： | 夏玉成,樊怀仁,胡明星,刘铁铭.霍州矿区断层构造的分形特征[J].西安科技大学学报,1997(1). |
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| 作者姓名： | 夏玉成 樊怀仁 胡明星 刘铁铭 |
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| 作者单位： | 西安矿业学院地质系 |
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| 摘 要： | 霍州矿区断层构造的分形特征与渭河盆地东区基本相同，都形成于张扭性的动力学环境；矿区内各井田的断层分维值以白龙井田最高，团柏井田最低；分维值的大小体现断层构造的复杂程度。
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| 关 键 词： | 分形 分维 断层 霍州矿区 |
FRACTAL CHARACTERISTICS OF FAULT STRUCTURES IN HUOZHOU MINING AREA |
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| Xia Yucheng,Fan Huairen,Hu Mingxing,Liu Tieming.FRACTAL CHARACTERISTICS OF FAULT STRUCTURES IN HUOZHOU MINING AREA[J].JOurnal of XI’an University of Science and Technology,1997(1). |
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| Authors: | Xia Yucheng Fan Huairen Hu Mingxing Liu Tieming |
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| Abstract: | The fractal characteristics of fault structures in Huozhou Mining Area is similar to that in the eastern district of Weihe Basin,both formed in the tenso shear dynamic environment.The maximum fractal dimension occures in Bailong coal field and the minimum value in Tuanbai coal field.The magnitude of the tractal dimensions reflects complexity of the fault stractures. |
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| Keywords: | fractal fractal dimension fault Huozhou Mining Area |
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