| 中国大陆山系、断层系的分形分维探讨 |
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| 引用本文： | 朱晓华.中国大陆山系、断层系的分形分维探讨[J].地质力学学报,1999,5(2):45-50. |
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| 作者姓名： | 朱晓华 |
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| 作者单位： | 南京师范大学地理科学学院,南京,210097 |
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| 摘 要： | 本文以中国为例运用分形理论对山系、断层系及其关系进行了相关研究，不仅判定了山系、断层系的分形性质，探讨了二者分维的地学意义，而且根据分数维的相关性，深入进行了二者关系的探讨，并从一个新的角度探讨了断层系的形成机制。
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| 关 键 词： | 分数维 山系 断层系 |
| 收稿时间： | 1998/11/12 0:00:00 |
| 修稿时间： | 1998-11-12 |
FRACTAL ANALYSIS OF MOUNTAIN RANGES AND FAULTS IN CHINA |
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| ZHU Xiaohua.FRACTAL ANALYSIS OF MOUNTAIN RANGES AND FAULTS IN CHINA[J].Journal of Geomechanics,1999,5(2):45-50. |
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| Authors: | ZHU Xiaohua |
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| Institution: | College of geographical Science, Nanjing Normal University 210097 |
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| Abstract: | A fractal and statistical analysis of mountain ranges and faults has been made respectively for southwest China and the whole continental area of China. It is found that the fractal dimension is 1.63 for mountain ridges in continental area of China, and 1.35 for those in southwest China. The fractal dimension is 1.65 for mountain ranges or faults indicates the difference of the frequency of distribution of mountain ridges or faults. The higher frequency of long mountain ranges or faults in southwest China than in the whole continental area of China, leads to the smaller fractal dimension of mountain ridges or faults in southwest China than in the whole continental area of China. It is concluded that both faults and mountain ridges are results of tectonic movements. |
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| Keywords: | fractal dimension mountain ridges faults |
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