| 水系展布方式与断裂活动程度的关系 |
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| 引用本文： | 尹克坚.水系展布方式与断裂活动程度的关系[J].华南地震,1991,11(1):41-45. |
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| 作者姓名： | 尹克坚 |
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| 作者单位： | 广西区地震办公室 |
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| 摘 要： | 作者在研究中发现水系的展布集中于区域内主要的活动断裂带方向及其正交方向上，并且断裂带活动程度越高，这种集中越明显，在文中，运用岩石破裂试验结果及水系展布受构造活动影响的观点对此进行讨论。
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| 关 键 词： | 地震地质 断裂活动 水系展布关系 岩石破裂试验 |
THE RELATIONS BETWEEN THE STRETCH OF RIVER SYSTEM AND FAULT ACTIVITY |
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| Yin Kejian Seismologic Office of Guangxi.THE RELATIONS BETWEEN THE STRETCH OF RIVER SYSTEM AND FAULT ACTIVITY[J].South China Journal of Seismology,1991,11(1):41-45. |
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| Authors: | Yin Kejian Seismologic Office of Guangxi |
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| Institution: | Yin Kejian Seismologic Office of Guangxi |
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| Abstract: | In this paper, some results of rock repture experiment and
the fact that river system is controlled dy structural movement are used to explain the relations and some results are gotten show ing in the following. 1. River system is controlled by main active fault zone and its strecth gathers in fault direction and its vertical direction. 2. The extent of this gathering becomes higher when the active extent of fault zone getting higher. |
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| Keywords: | Seismogeology The relations between the stretch of river system and fault activity |
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